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  <front>
    <journal-meta><journal-id journal-id-type="publisher">ACP</journal-id><journal-title-group>
    <journal-title>Atmospheric Chemistry and Physics</journal-title>
    <abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title><abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
  </journal-title-group><issn pub-type="epub">1680-7324</issn><publisher>
    <publisher-name>Copernicus Publications</publisher-name>
    <publisher-loc>Göttingen, Germany</publisher-loc>
  </publisher></journal-meta>
    <article-meta>
      <article-id pub-id-type="doi">10.5194/acp-21-6945-2021</article-id><title-group><article-title>Laboratory study of the collection efficiency of submicron aerosol particles
by cloud droplets – Part I: Influence of relative humidity</article-title><alt-title>Influence of relative humidity</alt-title>
      </title-group><?xmltex \runningtitle{Influence of relative humidity}?><?xmltex \runningauthor{A.~D\'{e}p\'{e}e et al.}?>
      <contrib-group>
        <contrib contrib-type="author" corresp="no" rid="aff1 aff2">
          <name><surname>Dépée</surname><given-names>Alexis</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="yes" rid="aff1">
          <name><surname>Lemaitre</surname><given-names>Pascal</given-names></name>
          <email>pascal.lemaitre@irsn.fr</email>
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff1">
          <name><surname>Gelain</surname><given-names>Thomas</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2 aff3">
          <name><surname>Monier</surname><given-names>Marie</given-names></name>
          
        </contrib>
        <contrib contrib-type="author" corresp="no" rid="aff2 aff3">
          <name><surname>Flossmann</surname><given-names>Andrea</given-names></name>
          
        <ext-link>https://orcid.org/0000-0002-4484-6425</ext-link></contrib>
        <aff id="aff1"><label>1</label><institution>Institut de Radioprotection et de Sûreté
Nucléaire (IRSN), PSN-RES, SCA, Gif-sur-Yvette, 91192,
France</institution>
        </aff>
        <aff id="aff2"><label>2</label><institution>Université Clermont Auvergne, Laboratoire de
Météorologie Physique, Clermont-Ferrand, France</institution>
        </aff>
        <aff id="aff3"><label>3</label><institution>CNRS, INSU, UMR 6016, LaMP, Aubière,
France</institution>
        </aff>
      </contrib-group>
      <author-notes><corresp id="corr1">Pascal Lemaitre (pascal.lemaitre@irsn.fr)</corresp></author-notes><pub-date><day>6</day><month>May</month><year>2021</year></pub-date>
      
      <volume>21</volume>
      <issue>9</issue>
      <fpage>6945</fpage><lpage>6962</lpage>
      <history>
        <date date-type="received"><day>6</day><month>August</month><year>2020</year></date>
           <date date-type="rev-request"><day>26</day><month>August</month><year>2020</year></date>
           <date date-type="rev-recd"><day>1</day><month>February</month><year>2021</year></date>
           <date date-type="accepted"><day>26</day><month>February</month><year>2021</year></date>
      </history>
      <permissions>
        <copyright-statement>Copyright: © 2021 Alexis Dépée et al.</copyright-statement>
        <copyright-year>2021</copyright-year>
      <license license-type="open-access"><license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri" xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p></license></permissions><self-uri xlink:href="https://acp.copernicus.org/articles/21/6945/2021/acp-21-6945-2021.html">This article is available from https://acp.copernicus.org/articles/21/6945/2021/acp-21-6945-2021.html</self-uri><self-uri xlink:href="https://acp.copernicus.org/articles/21/6945/2021/acp-21-6945-2021.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/21/6945/2021/acp-21-6945-2021.pdf</self-uri>
      <abstract><title>Abstract</title>
    <p id="d1e131">A new In-Cloud Aerosol Scavenging Experiment (In-CASE) has been conceived to
measure the collection efficiency (CE) of submicron aerosol particles by
cloud droplets. In this setup, droplets fall at their terminal velocity
through a 1 m high chamber in a laminar flow containing aerosol
particles. At the bottom of the In-CASE chamber, the droplet train is
separated from the aerosol particle flow – droplets are collected in an
impaction cup, whereas aerosol particles are deposited on a high-efficiency
particulate air (HEPA) filter. The collected droplets and the filter are
then analysed by fluorescence spectrometry since the aerosol particles are
atomised from a sodium fluorescein salt solution
(<inline-formula><mml:math id="M1" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">C</mml:mi><mml:mn mathvariant="normal">20</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">10</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">Na</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">5</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>). In-CASE fully controls all the parameters
which affect the CE – the droplets and aerosol particles size distributions
are monodispersed, the electric charges of droplets and aerosol particles
are controlled, and the relative humidity is indirectly set via the
chamber's temperature. This novel In-CASE setup is presented here as well as
the first measurements obtained to study the impact of relative humidity on
CE. For this purpose, droplets and particles are electrically neutralised. A
droplet radius of <inline-formula><mml:math id="M2" display="inline"><mml:mrow><mml:mn mathvariant="normal">49.6</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">1.3</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M3" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m has been considered for six
particle dry radii between 50 and 250 nm and three relative humidity levels
of <inline-formula><mml:math id="M4" display="inline"><mml:mrow><mml:mn mathvariant="normal">71.1</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">1.3</mml:mn></mml:mrow></mml:math></inline-formula> %, <inline-formula><mml:math id="M5" display="inline"><mml:mrow><mml:mn mathvariant="normal">82.4</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">1.4</mml:mn></mml:mrow></mml:math></inline-formula> % and <inline-formula><mml:math id="M6" display="inline"><mml:mrow><mml:mn mathvariant="normal">93.5</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">0.9</mml:mn></mml:mrow></mml:math></inline-formula> %. These new
CE measurements have been compared to theoretical models from literature
which adequately describe the relative humidity influence on the measured
CE.</p>
  </abstract>
    </article-meta>
  </front>
<body>
      

<sec id="Ch1.S1" sec-type="intro">
  <label>1</label><title>Introduction</title>
      <p id="d1e226">Every year, several billion tonnes of particulate matter are emitted in the
atmosphere, originating mainly from oceans, soils, gas-to-particle
conversion, evaporating clouds and from human activities (Jaenicke, 1993).
During the last decades, the life cycle of these aerosol particles (APs) has
been a key topic in atmospheric science for many reasons. First, APs play a
key role in weather and climate. They act on cloud formation, and their
chemical composition, size distribution and number concentration affect the
droplet size distributions and precipitation (Tao et al., 2012). They also
have an impact on the cloud cover, which in turn modulates albedo (Twomey et
al., 1974) – influencing the Earth's energy budget. Moreover, anthropogenic
APs have also been reported to impact human health (Dockery et al., 1992). In
fact, the Great Smog of London in 1952, one of the best-known related
events, caused up to 12 000 deaths (Bell et al., 2004). Radioactive material
released from a nuclear accident is another AP pollution hazard. Indeed,
many studies revealed that radioactive material like caesium-137 isotopes
can attach to the atmospheric APs and were transported over long distances
on a continental scale both after the Chernobyl (Devell et al., 1986; Jost
et al., 1986; Pölläen et al., 1997) and the Fukushima (Kaneyasu et
al., 2012; Adachi et al., 2013) nuclear accidents in 1986 and 2011,
respectively. With a half-life of up to 10 years, caesium-137 can remain
for decades in the atmosphere – following resuspension cycles of the
atmospheric APs – and jeopardise both ecosystems and human health.</p>
      <?pagebreak page6946?><p id="d1e229"><?xmltex \hack{\newpage}?>Thus, it is essential to understand the two mechanisms which move
atmospheric APs back to the ground. APs can settle through many effects like
gravity, wind, surface forces and turbulence. This is referred to as dry AP
deposition. There is also the wet AP deposition due to the interactions
between APs and clouds or their precipitations. The present paper deals with
the wet removal since, far away from the source, it is the main mechanism
involved in the AP scavenging (Jaenicke, 1993). Note that Flossmann (1998)
numerically showed that the wet deposition is mainly induced by the in-cloud
AP collection since 70 % of the AP mass contained in raindrops reaching
the soil comes from the cloud. This result is consistent with the
environmental measurements of Laguionie et al. (2014), who evaluated the
cloud contribution up to 60 % in the wet AP deposition. The in-cloud AP
scavenging is subdivided into two mechanisms – AP activation to form cloud
hydrometeors and AP collection by clouds hydrometeors. The in-cloud AP
collection is therefore a fundamental climate, weather and health issue. In
most of current AP wet removal models – like DESCAM (Detailed Scavenging
Model, Flossmann, 1985) – the AP collection is described through a
microphysical parameter called “collection efficiency” (CE), which
quantifies the ability of a droplet to capture the APs present in its
surroundings during its fall. It is the ratio between the AP number (or
mass) collected by the droplet over the AP number (or mass) within the
volume swept by the droplet for a given AP radius. Another equivalent
definition is the ratio of the cross-sectional area inside which the AP
trajectories are collected by the droplet over the cross-sectional area of
the droplet.</p>
      <p id="d1e233">Many microphysical effects influence this CE, and their contribution is
mainly dependent on the AP size. To be collected an AP has to deviate from
the streamline around the falling droplet to make contact with it. The
nanometric AP's trajectory is affected by the collisions with air molecules
– referred to as the Brownian diffusion. It results in random movement patterns
(see Fig. 1a) which tend to increase the CE when the AP radius
decreases. For massive APs, there is an increase in CE as they retain an
inertia strong enough to deviate significantly from the streamline when it
curves and to move straight toward the droplet surface – known as inertial
impaction (see Fig. 1b). When considering intermediate AP size, the CE
goes through a minimum value called the “Greenfield gap” (Greenfield,
1957) where the AP diffusion and inertia are weaker. In this gap, other
microphysical effects can be involved to make the droplet encounter the AP,
like the interception for instance. It is the collection of APs following a
streamline that approaches the droplet within a distance equivalent to the
particle radii (<inline-formula><mml:math id="M7" display="inline"><mml:mi>a</mml:mi></mml:math></inline-formula>) – see Fig. 1c. Note that the electrostatic forces
can have a significant influence on the CE (Tinsley and Zhou, 2015;
Dépée et al., 2019). This effect will be discussed in a companion
paper (Dépée et al., 2021) of this work.</p>
      <p id="d1e243">There are also thermophoretic and diffusiophoretic effects which can
influence the CE. In clouds, they shall favour the CE increase when
evaporation occurs and decrease CE during condensation (due to a thermal
equilibrium between the droplet and the air). Thermophoresis exists when a
thermal gradient prevails between the air and the droplet. When the relative
humidity (RH) is below 100 %, the evaporating droplet's surface
temperature (<inline-formula><mml:math id="M8" display="inline"><mml:mrow><mml:msub><mml:mi>T</mml:mi><mml:mtext>d,s</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) is colder than the bulk air temperature (<inline-formula><mml:math id="M9" display="inline"><mml:mrow><mml:msub><mml:mi>T</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>).
The average kinetic energy of air molecules is then decreasing when
approaching the droplet's surface. An AP is thus attracted by a
thermophoretic force near the evaporating droplet (see Fig. 1f) caused
by the asymmetry in kinetic energy transferred during each collision.
Diffusiophoresis occurs in an environment where a gradient of vapour density
in the air exists such as in the surrounding of an evaporating droplet. In
this case, water molecules diffuse toward the surrounding air while the
air molecules diffuse toward the droplet surface. In clouds, since the water
molar mass is lower than the air molar mass, there is an asymmetry in the
momentum transferred to APs close to the evaporating droplet produced by
collisions with the molecules from the continuous phase. This diffusion
tends to attract the AP to the droplet. Nonetheless, in order to maintain a
constant air pressure at the droplet surface, a hydrodynamical flow directed
toward the air is induced – this is the Stefan flow. The hydrodynamical drag
induced by the Stefan flow tends to repulse APs from an evaporating droplet.
Diffusiophoresis is the sum of the drag force produced by the Stefan flow and
the momentum transferred to APs (located in a diffusion boundary layer), due
to the dissymmetry of molecular weight. Note that the Stefan flow (repulsive
around an evaporating cloud droplet) is on average 5 times larger than
the addition to the diffusion flows (attractive around an evaporating cloud
droplet) as mentioned by Santachiara et al. (2012). So, diffusiophoresis
repulses APs from the evaporating droplet (see Fig. 1d), which in turn
decreases the CE. Finally, since the amplitude of the thermophoresis is on
average twice as large as the diffusiophoresis (Tinsley et al., 2006), APs
are ultimately attracted toward droplets in subsaturated air due to these
phoretic effects (see Fig. 1e). Thus, the coupling of the thermophoresis
and diffusiophoresis increases the CE when the relative humidity decreases.</p>
      <p id="d1e269">The influence of the relative humidity on the CE is described by the
well-known Wang et al. (1978) model, which is used in many cloud models like
DESCAM (Flossmann, 1985). Since their model predicts an important
contribution of thermophoresis and diffusiophoresis on the CE for cloud
droplet radii (<inline-formula><mml:math id="M10" display="inline"><mml:mrow><mml:mi>A</mml:mi><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">100</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M11" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m) and submicron AP radii, it is
desirable to validate those theoretical CEs through experiments. A review of
available CE measurements can be found in Ardon-Dryer et al. (2015). The
only experimental study that tackles the influence of the relative humidity
on the CE for cloud droplets is the one of Ardon-Dryer et al. (2015), which
tested two levels of relative humidity of 15 % and 88 %. However, in their
work they report that the measured electric charge on the droplets were <inline-formula><mml:math id="M12" display="inline"><mml:mrow><mml:mn mathvariant="normal">400</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">400</mml:mn></mml:mrow></mml:math></inline-formula> elementary charges, and on the APs they were 1 elementary charge.
Therefore,<?pagebreak page6947?> the electrostatic forces should have had a significant influence
on the measured CE for the droplet radius considered (<inline-formula><mml:math id="M13" display="inline"><mml:mrow><mml:mi>A</mml:mi><mml:mo>≈</mml:mo><mml:mn mathvariant="normal">21.6</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M14" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m) as numerically shown by Tinsley and Zhou (2015). Furthermore, there
are no similar measurements for other cloud droplet sizes either for high
levels of relative humidity as found in cloud.</p>
      <p id="d1e324">The purpose of this work is to fill up the deficiency of data in this area.
Thus, a novel experiment has been developed in order to study the influence
of the relative humidity on the CE to assess the magnitude of the
thermophoretic and diffusiophoretic processes. With this experiment, the
influence of electric charges can also be investigated, and this is the
objective of the companion paper (Dépée et al., 2021).</p>
      <p id="d1e327">After the introduction, the experimental setup is detailed, while
the experimental method to evaluate the CE and the uncertainties are
described in Sect. 3. Section 4 is dedicated to the new CE
measurements which are presented and compared to theoretical data from the
Wang et al. (1978) Eulerian model. Another comparison is made in the last
section to the newer Lagrangian model of Dépée et al. (2019) since
it can model every microphysical effect involved in the AP collection by
cloud droplets (like Brownian motion, inertial impaction and interception) and especially their coupling. Dépée et al. (2019) focused on
the electrostatic forces but did not consider the thermophoresis and the
diffusiophoresis. Here, we extend the Dépée et al. (2019) model by
adding these phoretic effects. Finally, this study experimentally validates
the Dépée et al. (2019) model, which provides consistent theoretical
CEs for a convenient incorporation in cloud models, pollution models,
climate models and so forth.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F1" specific-use="star"><?xmltex \currentcnt{1}?><?xmltex \def\figurename{Figure}?><label>Figure 1</label><caption><p id="d1e332">AP trajectories computed with the extended Dépée et al. (2019) model for a 50 <inline-formula><mml:math id="M15" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m droplet radius (<inline-formula><mml:math id="M16" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>) and AP with various radii
(<inline-formula><mml:math id="M17" display="inline"><mml:mi>a</mml:mi></mml:math></inline-formula>) and densities (<inline-formula><mml:math id="M18" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">ρ</mml:mi><mml:mtext>AP</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>). The air temperature (<inline-formula><mml:math id="M19" display="inline"><mml:mrow><mml:msub><mml:mi>T</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) and the
air pressure (<inline-formula><mml:math id="M20" display="inline"><mml:mrow><mml:msub><mml:mi>P</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) are <inline-formula><mml:math id="M21" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>17 <inline-formula><mml:math id="M22" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C and 540 hPa respectively. The
panels indicate the effects of Brownian motion <bold>(a)</bold>, inertial impact <bold>(b)</bold>,
interception <bold>(c)</bold>, diffusiophoresis <bold>(d)</bold>, combined thermophoresis and
diffusiophoresis <bold>(e)</bold>, and thermophoresis <bold>(f)</bold>. Red trajectories result in an
AP collection. <bold>(d, f)</bold> The gradients are equivalent to a relative
humidity of 0.01 % (when there is no gradient the equivalent relative
humidity is 100 %). <inline-formula><mml:math id="M23" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">ρ</mml:mi><mml:mtext>v,s</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M24" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">ρ</mml:mi><mml:mtext>v,air</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> are the vapour
densities at the droplet surface and in the bulk air, respectively.</p></caption>
        <?xmltex \igopts{width=341.433071pt}?><graphic xlink:href="https://acp.copernicus.org/articles/21/6945/2021/acp-21-6945-2021-f01.png"/>

      </fig>

</sec>
<sec id="Ch1.S2">
  <label>2</label><title>Experimental setup</title>
<sec id="Ch1.S2.SS1">
  <label>2.1</label><title>Overview</title>
      <p id="d1e472">All measurements were conducted inside the In-Cloud Aerosol Scavenging
Experiment (In-CASE). Figure 2 shows the airflow diagram with the different
parts of the experiment in order to study the relative humidity influence on
the CE. The major In-CASE component is the collision chamber (Fig. 2)
where a laminar flow containing APs interacts with a train of droplets
falling at terminal velocity. In this chamber, the droplet and AP size
distributions are monodispersed, and for this particular work the droplet and
AP electric charges are neutralised. Droplets are generated through a
piezoelectric inductor and neutralised with an electrostatic inductor (detailed
in Sect. 2.4), and the radius is measured by optical shadowgraphy with a strobe and
a camera (brown, Fig. 2). In Fig. 2, orange shows the AP generation
(which is described in Sect. 2.3), black shows an exhaust used to
evacuate the AP flow rate surplus at the atomiser's outlet, red shows an
Argon flow injected into the In-CASE chamber's bottom part to separate
droplets from the AP flow (this is detailed in “AP and droplet separation” in Sect. 2.2.2) and purple indicates the AP flow which leaves the chamber toward a high-efficiency particulate air (HEPA) filter.</p>
      <p id="d1e475">The relative humidity in the collision chamber is set through the
temperature, with the latter being controlled via a cooling system. In the next
sections, the In-CASE chamber as well as the droplets and AP
characterisation are described.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F2"><?xmltex \currentcnt{2}?><?xmltex \def\figurename{Figure}?><label>Figure 2</label><caption><p id="d1e480">In-CASE setup to study the influence of relative humidity. Colours
represent different functions. Red represents upward Argon flow against AP pollution
in the droplet impaction cup. Purple represents AP (and Argon) evacuation toward the
HEPA filter. Orange represents AP, generation, selection and neutralisation. Black represents surplus evacuation and differential mobility analyser (DMA) flow rate control. Brown represents droplet radius
measurement. All the key features of the setup are detailed in Table 2.</p></caption>
          <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://acp.copernicus.org/articles/21/6945/2021/acp-21-6945-2021-f02.png"/>

        </fig>

</sec>
<sec id="Ch1.S2.SS2">
  <label>2.2</label><title>In-CASE chamber</title>
      <p id="d1e497">The In-CASE chamber (see Fig. 2) is subdivided into three stages – the
injection head, the collision chamber and the In-CASE chamber's bottom part.
These three parts will be detailed in the next subsections.</p>
<sec id="Ch1.S2.SS2.SSS1">
  <label>2.2.1</label><title>Injection head</title>
      <p id="d1e507">The injection head is composed of two parts – the droplets and the AP
injection. The upper part is used to inject the droplets while the APs are
injected in the second part about 10 cm below. This distance is required to
measure the droplet size through the two facing windows (see Sect. 2.4.1)
but also to let droplets decelerate and reach their terminal velocity.</p>
      <p id="d1e510">The droplet train is injected through a housing made with a 3D printer set
at the top of the droplet injector (see Fig. 3). This housing has been
constructed to precisely place the droplet generator and the electrostatic
inductor together. Indeed, the electrostatic inductor has to keep the same
position relative to the droplet generator to prevent changes in the
electric field <inline-formula><mml:math id="M25" display="inline"><mml:mrow><mml:msub><mml:mi>E</mml:mi><mml:mtext>ind</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>, which in turn can disturb the droplet charge and
stop the neutralisation (detailed in Sect. 2.4.2).</p>
      <p id="d1e524">The APs are injected from the sides of the entire circumference through a
flat torus inlet. This injection principle is based on the CLINCH experiment
(CoLlision Ice Nucleation CHamber, Ladino et al., 2011), which ensures a
laminar flow and a great spatial APs mixture in the collision chamber's
inlet.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F3"><?xmltex \currentcnt{3}?><?xmltex \def\figurename{Figure}?><label>Figure 3</label><caption><p id="d1e530">View of the In-CASE chamber's top with the injection head where APs
and droplets are injected into the collision chamber.</p></caption>
            <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://acp.copernicus.org/articles/21/6945/2021/acp-21-6945-2021-f03.png"/>

          </fig>

</sec>
<sec id="Ch1.S2.SS2.SSS2">
  <label>2.2.2</label><title>In-CASE bottom stage</title>
      <p id="d1e547">The CE is calculated from the AP mass collected by the droplets during an
experiment and the average AP mass concentration in the collision chamber.
To obtain these quantities, the droplet train must be separated from the
interstitial APs (which were not collected).</p>
</sec>
<sec id="Ch1.S2.SS2.SSSx1" specific-use="unnumbered">
  <title>AP and droplet separation</title>
      <p id="d1e556">The system developed to separate the droplet train from the AP flow is
presented in Fig. 4. It is composed of a converging portion (from 5 to 3 cm in diameter) where a gutter is inserted to prevent the water condensed on
the wall from entering to the In-CASE chamber bottom. The APs are directly
vacuumed toward a HEPA filter (see Fig. 2) at the upper part of the
separator through four outlets while the droplets – containing collected APs
– are impacted into a cup at the separator's lower part.</p>
      <?pagebreak page6948?><p id="d1e559">To prevent AP pollution in the droplet impaction cup, a counterflow is
injected below the In-CASE chamber and passes through the droplet
impaction cup from nine holes set on its entire circumference. Since the
counterflow is injected at the laboratory temperature, and the AP downward
flow is colder, Argon – denser than the air – was selected to avoid any
Rayleigh–Taylor instability (Sharp, 1983).</p>
      <p id="d1e562">Argon is injected at 0.4 L min<inline-formula><mml:math id="M26" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>. The diameter of the nine holes is 4 mm, and
the top of the droplet impaction cup is 2.5 cm. Thus, the upward Argon flow
is injected at 5.9 and 1.4 cm s<inline-formula><mml:math id="M27" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>, through the nine holes and the top of the
impaction cup, respectively. Because the droplet velocity is about 25 cm s<inline-formula><mml:math id="M28" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>
(for the 50 <inline-formula><mml:math id="M29" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m droplet radius studied) and the AP terminal velocity is
less than 10<inline-formula><mml:math id="M30" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> cm s<inline-formula><mml:math id="M31" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>, APs cannot settle into the impaction cup, whereas
droplets are impacted without undue disruption.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F4"><?xmltex \currentcnt{4}?><?xmltex \def\figurename{Figure}?><label>Figure 4</label><caption><p id="d1e636">View of the In-CASE chamber's bottom – AP and droplet separation.</p></caption>
            <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://acp.copernicus.org/articles/21/6945/2021/acp-21-6945-2021-f04.png"/>

          </fig>

</sec>
<sec id="Ch1.S2.SS2.SSSx2" specific-use="unnumbered">
  <title>Validation</title>
      <p id="d1e652">The droplet and AP separation were verified with two tests. First, In-CASE
was run under standard experimental conditions except no droplets were
generated. After 5 h of experiment, a spectrometry analysis was
performed in the droplet impaction cup, and no fluorescein was detected.
Thus, no AP had settled on the droplet impaction cup during the experiment.</p>
      <p id="d1e655">The second test was to ensure that droplets were collected by the impaction
cup. Then, In-CASE was again run like a typical experiment except the flow
passing through the In-CASE chamber was clean air without any AP. Droplets
were tracked by adding sodium fluorescein salt in the water supplying the
piezoelectric injector. Since the concentration of sodium fluorescein salt
in the water, the droplet generation frequency, the droplet size and the
experiment time were known, the goal was to verify if the expected
fluorescein mass in the droplets and the actual measured fluorescein mass
were equal. After 5 h (<inline-formula><mml:math id="M32" display="inline"><mml:mrow><mml:mo>=</mml:mo><mml:mn mathvariant="normal">450</mml:mn></mml:mrow></mml:math></inline-formula> 000 injected droplets), a discrepancy
of 2 % between expected and measured fluorescein mass was obtained.
Therefore, all droplets are considered impacted in the impaction cup.</p>
      <p id="d1e668">Finally, this indicates that the AP mass detected in the droplet impaction
cup after the experiment effectively results from collection by drops in the
In-CASE collision chamber and not from contamination from other sources.</p>
</sec>
<?pagebreak page6949?><sec id="Ch1.S2.SS2.SSS3">
  <label>2.2.3</label><title>Collision chamber</title>
      <p id="d1e679">The collision chamber is a 1 m stainless steel cylinder with an inner
diameter of 5 cm (see Fig. 5). The collision chamber's temperature is
controlled through a coolant which spirally circulates outside the chamber,
from the bottom to the top of the collision chamber. The pressure
(<inline-formula><mml:math id="M33" display="inline"><mml:mrow><mml:msub><mml:mi>P</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>), temperature (<inline-formula><mml:math id="M34" display="inline"><mml:mrow><mml:msub><mml:mi>T</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) and relative humidity (RH) are
measured at the top and the bottom by sensors. To clean the chamber, water
or compressed dried air is injected via a purge. Three sampling points are
available but were not used for these experiments.</p>
      <p id="d1e704">The temperature and the relative humidity discrepancies between top and
bottom were respectively less than 1 <inline-formula><mml:math id="M35" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C and 4 % in all the CE
measurements – the mean values are then considered for both parameters.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F5"><?xmltex \currentcnt{5}?><?xmltex \def\figurename{Figure}?><label>Figure 5</label><caption><p id="d1e718">In-CASE collision chamber – 2D section plane.</p></caption>
            <?xmltex \igopts{width=142.26378pt}?><graphic xlink:href="https://acp.copernicus.org/articles/21/6945/2021/acp-21-6945-2021-f05.png"/>

          </fig>

</sec>
<sec id="Ch1.S2.SS2.SSSx3" specific-use="unnumbered">
  <title>Thermodynamic conditions</title>
      <p id="d1e733">All the experiments were conducted at atmospheric pressure. To get
comparable CE measurements, the temperature has been set to <inline-formula><mml:math id="M36" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.58</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">0.50</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M37" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C – as constant as possible between experiments. Three
levels of relative humidity (RH) were considered – 71.1 %, 82.4 % and
93.5 %. To increase the relative humidity at a given collision chamber
temperature, the temperature of the pure water in the humidifier (Fig. 2)
was increased. The relative humidity level of 71.1 % was obtained by
completely removing the humidifier to get the driest AP flow possible at the
collision chamber's inlet. At lab temperature (about 22 <inline-formula><mml:math id="M38" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C), the
relative humidity of the dry AP flow ranged from 10 % to 20 % at the
In-CASE chamber inlet.</p>
      <p id="d1e766">Note that the AP flow before the injection head is also thermally set to
inject APs with the same temperature as in the collision chamber.</p><?xmltex \hack{\newpage}?>
</sec>
<?pagebreak page6950?><sec id="Ch1.S2.SS2.SSSx4" specific-use="unnumbered">
  <title>Droplet evaporation</title>
      <p id="d1e776">The change in droplet radius due to evaporation in the collision chamber is
calculated according to the Sect. 13.2 of Pruppacher and Klett (1997). The
corresponding terminal velocity (<inline-formula><mml:math id="M39" display="inline"><mml:mrow><mml:msub><mml:mi>U</mml:mi><mml:mrow><mml:mi>A</mml:mi><mml:mo>,</mml:mo><mml:mi mathvariant="normal">∞</mml:mi></mml:mrow></mml:msub><mml:mo>≈</mml:mo><mml:mn mathvariant="normal">25</mml:mn></mml:mrow></mml:math></inline-formula> cm s<inline-formula><mml:math id="M40" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>) is computed from Beard (1976). The residence time of the droplet
in the chamber (<inline-formula><mml:math id="M41" display="inline"><mml:mrow><mml:mo>≈</mml:mo><mml:mn mathvariant="normal">4</mml:mn></mml:mrow></mml:math></inline-formula> s) is computed considering these two changes.
Since the droplet radius only decreases around 3 % by evaporation with
the lower relative humidity considered in the experiments (71.1 %), the
droplet evaporation in the collision chamber is neglected.</p>
</sec>
<sec id="Ch1.S2.SS2.SSSx5" specific-use="unnumbered">
  <title>AP hygroscopicity</title>
      <p id="d1e827">The APs are composed of pure sodium fluorescein salt, which is a high
hygroscopic chemical compound. The APs inside the collision chamber then
grow to reach their equilibrium size with the relative humidity (RH). In
order to evaluate the increase in size by humidification, the AP growth
factor (GroF) measured in Quérel et al. (2014) was considered. The
growth factor is defined as the ratio of the size of the wet AP over the
size of the dry AP. Since their data are limited to relative humidity levels
below 90 %, the kappa theory described in Petters and Kreidenweis (2007)
is used to extrapolate to the required values. To fit the measurements of
Quérel et al. (2014) with the kappa theory, only their data with a
relative humidity level less than 85 % were considered. Figure 6 shows
the AP growth factor related to the relative humidity for a kappa value of
0.23 and two extreme values of 0.2 and 0.27 – fitting to the sodium
fluorescein salt hygroscopicity.</p>
      <p id="d1e830">Thus, for relative humidity levels of 71.1 %, 82.4 % and 93.5 %
studied here, a dry AP radius of 50 nm selected by the differential mobility analyser (DMA) grows with a
growth factor (GroF) of 1.16, 1.27 and 1.57, respectively. Consequently,
the CEs measured are applied for size of respectively 58.0, 63.5 and 78.5 nm AP radii.</p>
      <p id="d1e833">Note that the AP density is not the one of sodium fluorescein salt (<inline-formula><mml:math id="M42" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">ρ</mml:mi><mml:mtext>fluorescein</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1580</mml:mn></mml:mrow></mml:math></inline-formula> kg m<inline-formula><mml:math id="M43" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>) since APs contain water. Indeed,
the water density (<inline-formula><mml:math id="M44" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">ρ</mml:mi><mml:mtext>water</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) should be considered in the AP density
(<inline-formula><mml:math id="M45" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">ρ</mml:mi><mml:mtext>AP</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) calculation. At a given relative humidity (RH), the AP
density inside the chamber is then deduced by Eq. (1):
              <disp-formula id="Ch1.E1" content-type="numbered"><label>1</label><mml:math id="M46" display="block"><mml:mrow><mml:msub><mml:mi mathvariant="italic">ρ</mml:mi><mml:mtext>AP</mml:mtext></mml:msub><mml:mfenced close=")" open="("><mml:mtext>RH</mml:mtext></mml:mfenced><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi mathvariant="italic">ρ</mml:mi><mml:mtext>fluorescein</mml:mtext></mml:msub><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="italic">ρ</mml:mi><mml:mtext>water</mml:mtext></mml:msub><mml:mo>×</mml:mo><mml:mfenced close="]" open="["><mml:mrow><mml:mtext>GroF</mml:mtext><mml:msup><mml:mfenced open="(" close=")"><mml:mtext>RH</mml:mtext></mml:mfenced><mml:mn mathvariant="normal">3</mml:mn></mml:msup><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:mfenced></mml:mrow><mml:mrow><mml:mi mathvariant="normal">GroF</mml:mi><mml:msup><mml:mfenced open="(" close=")"><mml:mi mathvariant="normal">RH</mml:mi></mml:mfenced><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>.</mml:mo></mml:mrow></mml:math></disp-formula></p>
      <p id="d1e942">Since the relative humidity after the dryer (see Fig. 2) ranges from 10 % to
20 %, the AP growth factor is less than 1.02 (see Fig. 6) in the DMA.
APs are then considered dry when exiting the DMA.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F6"><?xmltex \currentcnt{6}?><?xmltex \def\figurename{Figure}?><label>Figure 6</label><caption><p id="d1e948">Growth factor (GroF) as function of the given relative humidity
(RH). Data points (dots) from Quérel et al. (2014) and fits (lines)
with the kappa theory (Petters and Kreidenweis, 2007).</p></caption>
            <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://acp.copernicus.org/articles/21/6945/2021/acp-21-6945-2021-f06.png"/>

          </fig>

</sec>
</sec>
<sec id="Ch1.S2.SS3">
  <label>2.3</label><title>AP generation</title>
      <p id="d1e966">APs are generated by the atomisation (atomiser, TSI 3076) of a sodium
fluorescein salt solution (<inline-formula><mml:math id="M47" display="inline"><mml:mrow class="chem"><mml:msub><mml:mi mathvariant="normal">C</mml:mi><mml:mn mathvariant="normal">20</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">H</mml:mi><mml:mn mathvariant="normal">10</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">Na</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:msub><mml:mi mathvariant="normal">O</mml:mi><mml:mn mathvariant="normal">5</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>). This molecule
has been selected for its significant fluorescent<?pagebreak page6951?> properties, detectable at
very low concentrations (down to 10<inline-formula><mml:math id="M48" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">10</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> g L<inline-formula><mml:math id="M49" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>). Once atomised, the fine
droplets go through a dry diffuser to produce dry APs. In Fig. 7, two AP
size distributions are presented for two different concentrations of the
sodium fluorescein salt solution considered – 36 and 100 g L<inline-formula><mml:math id="M50" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> – during the
experiments. Those two size distributions have been evaluated using a
scanning mobility particle sizer (SMPS). It was observed that the size
distribution mode passes from 41 to 67.9 nm in radius when the concentration
becomes 3 times larger. Since the geometric standard deviation (<inline-formula><mml:math id="M51" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">σ</mml:mi><mml:mtext>g</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) is above 1.75, a differential mobility analyser (DMA; TSI 3080) is
set between the atomiser and the In-CASE chamber to reduce the dispersion
of the AP size distribution. After exiting the DMA, the AP flow goes through
a low-energy X-ray neutraliser (<inline-formula><mml:math id="M52" display="inline"><mml:mo lspace="0mm">&lt;</mml:mo></mml:math></inline-formula> 9.5 keV, TSI 3088) so that the AP
charge distribution entering the In-CASE chamber is similar to a Boltzmann
distribution. After the neutralisation, the dry AP flow is humidified by a
pure water container in order to get high relative humidity in the collision
chamber.</p>
      <p id="d1e1050">Note that the DMA selects APs according to their electrical mobility – <inline-formula><mml:math id="M53" display="inline"><mml:mi>Z</mml:mi></mml:math></inline-formula> in Eq. (6) – assuming that only single charged APs can
leave the DMA. Actually, depending on the AP size distribution and the AP
flow rate in the DMA, larger AP radii carrying multiple charges than the one
considered can also be selected. Sometimes those multiple charged APs cannot
be neglected as discussed in Sect. 3.2.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F7" specific-use="star"><?xmltex \currentcnt{7}?><?xmltex \def\figurename{Figure}?><label>Figure 7</label><caption><p id="d1e1062">Two typical AP size distributions obtained with a SMPS at the
atomiser's outlet. The concentration of the sodium fluorescein salt solution
is 36 g L<inline-formula><mml:math id="M54" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> <bold>(a)</bold> and 100 g L<inline-formula><mml:math id="M55" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> <bold>(b)</bold>. <inline-formula><mml:math id="M56" display="inline"><mml:mrow><mml:msub><mml:mi>D</mml:mi><mml:mtext>max</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M57" display="inline"><mml:mrow><mml:msub><mml:mi>D</mml:mi><mml:mrow><mml:mn mathvariant="normal">50</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi mathvariant="italic">%</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula> are
respectively the maximum diameter selected by the DMA and the cut-off
diameter of the impactor at the DMA's inlet, at a given AP flow rate (0.6 L min<inline-formula><mml:math id="M58" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>).</p></caption>
          <?xmltex \igopts{width=398.338583pt}?><graphic xlink:href="https://acp.copernicus.org/articles/21/6945/2021/acp-21-6945-2021-f07.png"/>

        </fig>

</sec>
<sec id="Ch1.S2.SS4">
  <label>2.4</label><title>Droplet characterisation</title>
<sec id="Ch1.S2.SS4.SSS1">
  <label>2.4.1</label><title>Droplet generation frequency and size measurement</title>
      <p id="d1e1155">The droplet generator used for these experiments is a piezoelectric injector
provided by Microfab – the MJ-ABL-01 model with an internal diameter of 150 <inline-formula><mml:math id="M59" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m. This model has been used for its stability over time, since the
experiments can last up to 5 h. This piezoelectric injector generates
droplets – at a given frequency – above their terminal velocity. The
distance between two following droplets reduces when droplets fall away from
the injector's nozzle since the droplet velocity decreases (see Fig. 8,
left). It was emphasised during ex situ experiments that droplet generation
frequencies greater than 25 Hz induce droplet coalescence since the
inter-droplet space becomes too short to prevent droplets from
aerodynamically disturbing each other. This agrees with Ardon-Dryer et al. (2015), who observed droplet coalescence for droplet generation frequency
larger than 30 Hz operating a similar piezoelectric injector. Thus, droplets
were generated at 25 Hz  in all experiments presented in this current paper.</p>
      <p id="d1e1166">The droplet generator is placed at the top of the In-CASE collision
chamber, within an injection head (see Fig. 3). A few times during an
experiment, droplet pictures are recorded by optical shadowgraphy through
two facing windows in the injection head (see Fig. 3). A circle Hough
transform is then applied to evaluate the droplet radii in the recorded
pictures. An example is given in Fig. 8 (right) for a 49.7 <inline-formula><mml:math id="M60" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m droplet
radius. Note that the size distributions of the droplets generated by the
piezoelectric injector are considered monodispersed since the droplet size
dispersion is very low (<inline-formula><mml:math id="M61" display="inline"><mml:mrow><mml:mi mathvariant="italic">σ</mml:mi><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:math></inline-formula> %).</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F8"><?xmltex \currentcnt{8}?><?xmltex \def\figurename{Figure}?><label>Figure 8</label><caption><p id="d1e1191">(Left) Droplet train at the piezoelectric injector's outlet
obtained by optical shadowgraphy – the droplet generating frequency is 200 Hz. (Right) A droplet picture obtained by optical shadowgraphy – the droplet
radius and centre are detected through a circle Hough transform (red cross
and line).</p></caption>
            <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://acp.copernicus.org/articles/21/6945/2021/acp-21-6945-2021-f08.png"/>

          </fig>

</sec>
<sec id="Ch1.S2.SS4.SSS2">
  <label>2.4.2</label><title>Droplet charge neutralisation</title>
      <p id="d1e1208">It is well know that the piezoelectric droplet generator produces highly
electrically charged droplets. With a similar device, Ardon-Dryer et al. (2015) measured up to 10<inline-formula><mml:math id="M62" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> elementary charges on the generated droplets.
Since this paper focused only on the relative humidity influence, the
droplets, as well as APs, must be neutralised.</p>
      <p id="d1e1220">To do so, an electrostatic inductor was built following Reischl et al. (1977). Two parallel metal plates are placed at the droplet generator's
nozzle – this is the electrostatic inductor shown in Fig. 9 (labelled 1,
left). One plate is connected to a potential (<inline-formula><mml:math id="M63" display="inline"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mtext>ind</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) while the other is
connected to the neutral potential – as presented in Fig. 9 – in order to
induce an electric field (<inline-formula><mml:math id="M64" display="inline"><mml:mrow><mml:msub><mml:mi>E</mml:mi><mml:mtext>ind</mml:mtext></mml:msub><mml:mo>∼</mml:mo></mml:mrow></mml:math></inline-formula>10<inline-formula><mml:math id="M65" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:math></inline-formula>–10<inline-formula><mml:math id="M66" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:math></inline-formula> V m<inline-formula><mml:math id="M67" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>). Sodium
chloride is added to the pure water that feeds the piezoelectric injector.
According to the generated electric field polarity, the system can
selectively attract negative or positive ions toward the nozzle where the
droplet is formed. If <inline-formula><mml:math id="M68" display="inline"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mtext>ind</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is positive, the negative chloride ions
(Cl<inline-formula><mml:math id="M69" display="inline"><mml:msup><mml:mi/><mml:mo>-</mml:mo></mml:msup></mml:math></inline-formula>) migrate toward the nozzle and the positive sodium ions
(Na<inline-formula><mml:math id="M70" display="inline"><mml:msup><mml:mi/><mml:mo>+</mml:mo></mml:msup></mml:math></inline-formula>) are repulsed from the nozzle and inversely if the potential is
negative. Following the electric field amplitude – through <inline-formula><mml:math id="M71" display="inline"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mtext>ind</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> – the
ion quantity can be set. This system can conclusively control the droplet
charge. Note that the sodium chloride concentration has no effect on the
principle of induction used here since the ion number is large enough for
the entire experiment period (Reischl et al., 1977) – 3.3 g L<inline-formula><mml:math id="M72" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> has been
considered.</p>
      <p id="d1e1330">To evaluate the droplet charge and then neutralise the droplets, an ex situ
experiment has been conducted where the droplet train passed through a
capacitor (labelled 2, Fig. 9, left). One capacitor's plate is connected
to the neutral, whereas the other is connected to a high potential
(<inline-formula><mml:math id="M73" display="inline"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mtext>cap</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) – inducing an electric field (<inline-formula><mml:math id="M74" display="inline"><mml:mrow><mml:msub><mml:mi>E</mml:mi><mml:mtext>cap</mml:mtext></mml:msub><mml:mo>∼</mml:mo></mml:mrow></mml:math></inline-formula>10<inline-formula><mml:math id="M75" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">5</mml:mn></mml:msup></mml:math></inline-formula>–10<inline-formula><mml:math id="M76" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">6</mml:mn></mml:msup></mml:math></inline-formula> V m<inline-formula><mml:math id="M77" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>). A Faraday cage surrounding the capacitor and a plate maintained at a
neutral potential are set in order to prevent the electric field at the
capacitor (<inline-formula><mml:math id="M78" display="inline"><mml:mrow><mml:msub><mml:mi>E</mml:mi><mml:mtext>cap</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) from disturbing the electric field at the inductor
(<inline-formula><mml:math id="M79" display="inline"><mml:mrow><mml:msub><mml:mi>E</mml:mi><mml:mtext>ind</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>), which could change the droplet charge. Finally, the potential
<inline-formula><mml:math id="M80" display="inline"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mtext>ind</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> which electrically neutralises the droplet is found by selecting
for the <inline-formula><mml:math id="M81" display="inline"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mtext>ind</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> value which minimises the droplet train deflection.</p>
      <p id="d1e1432">Actually, this system can also be used to precisely evaluated the electric
charges on the droplets (for both polarities); this method is applied and
presented in Dépée et al. (2021).</p>
      <p id="d1e1436">Note that the droplet charge induced by the piezoelectric injector has been
calculated to
<inline-formula><mml:math id="M82" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>8400 elementary charges – in line with Ardon-Dryer et al. (2015) using a
similar generator. Moreover, after the droplet neutralisation, an
uncertainty of 600 elementary charges was estimated.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F9"><?xmltex \currentcnt{9}?><?xmltex \def\figurename{Figure}?><label>Figure 9</label><caption><p id="d1e1448">(Left) 1 – Electrostatic inductor set at the piezoelectric
injector's nozzle to electrically neutralise the droplets. 2 – Capacitor
used to analyse the droplet deviation caused by the electric field in the
capacitor (<inline-formula><mml:math id="M83" display="inline"><mml:mrow><mml:msub><mml:mi>E</mml:mi><mml:mtext>cap</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>). (Right) Housing made with a 3D printer containing the
piezoelectric injector and the electrostatic inductor, set in the injection
head (see Fig. 3).</p></caption>
            <?xmltex \igopts{width=142.26378pt}?><graphic xlink:href="https://acp.copernicus.org/articles/21/6945/2021/acp-21-6945-2021-f09.png"/>

          </fig>

</sec>
</sec>
</sec>
<?pagebreak page6952?><sec id="Ch1.S3">
  <label>3</label><title>Data analysis</title>
<sec id="Ch1.S3.SS1">
  <label>3.1</label><title>Definition of the collection efficiency</title>
      <p id="d1e1485">At the end of an experiment, the collection efficiency (CE) is calculated
from Eq. (2):
            <disp-formula id="Ch1.E2" content-type="numbered"><label>2</label><mml:math id="M84" display="block"><mml:mrow><mml:mi mathvariant="normal">CE</mml:mi><mml:mo>(</mml:mo><mml:mi mathvariant="normal">a</mml:mi><mml:mo>,</mml:mo><mml:mi mathvariant="normal">A</mml:mi><mml:mo>,</mml:mo><mml:mi mathvariant="normal">HR</mml:mi><mml:mo>)</mml:mo><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,d</mml:mtext></mml:msub></mml:mrow><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,available</mml:mtext></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where the AP mass collected by all droplets (<inline-formula><mml:math id="M85" display="inline"><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,d</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) is directly
measured by spectrometry analysis in the droplet impaction cup (see Fig. 4), while the mass of available APs in the volume swept by the droplets
(<inline-formula><mml:math id="M86" display="inline"><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,available</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) is given by Eq. (3):
            <disp-formula id="Ch1.E3" content-type="numbered"><label>3</label><mml:math id="M87" display="block"><mml:mtable rowspacing="0.2ex" class="split" columnspacing="1em" displaystyle="true" columnalign="right left"><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,available</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:mi mathvariant="italic">π</mml:mi><mml:msup><mml:mfenced open="(" close=")"><mml:mrow><mml:mi>A</mml:mi><mml:mo>+</mml:mo><mml:mtext>GroF(RH)</mml:mtext><mml:mo>×</mml:mo><mml:mi>a</mml:mi></mml:mrow></mml:mfenced><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mo>×</mml:mo><mml:msub><mml:mi>F</mml:mi><mml:mtext>d</mml:mtext></mml:msub></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:mo>×</mml:mo><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi>t</mml:mi><mml:mo>×</mml:mo><mml:msub><mml:mi>H</mml:mi><mml:mtext>eff</mml:mtext></mml:msub><mml:mo>×</mml:mo><mml:msub><mml:mi>C</mml:mi><mml:mtext>m,AP</mml:mtext></mml:msub><mml:mo>.</mml:mo></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula></p>
      <?pagebreak page6953?><p id="d1e1616"><inline-formula><mml:math id="M88" display="inline"><mml:mrow><mml:msub><mml:mi>F</mml:mi><mml:mtext>d</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M89" display="inline"><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi>t</mml:mi></mml:mrow></mml:math></inline-formula> are respectively the droplet generation frequency and the
experiment duration – the product of those two quantities is the number of
droplets injected during an experiment. <inline-formula><mml:math id="M90" display="inline"><mml:mrow><mml:msub><mml:mi>C</mml:mi><mml:mtext>m,AP</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is the mean AP mass
concentration in the In-CASE collision chamber. Note that <inline-formula><mml:math id="M91" display="inline"><mml:mi>a</mml:mi></mml:math></inline-formula> is the AP dry
radius corrected by the growth factor (GroF) which depends on the relative
humidity (see “AP hygroscopicity” in Sect. 2.2.3). <inline-formula><mml:math id="M92" display="inline"><mml:mrow><mml:msub><mml:mi>H</mml:mi><mml:mtext>eff</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is the effective height of
interaction between droplets and APs. Since the APs are also falling in the
In-CASE collision chamber, this height is not the In-CASE collision
chamber's height (<inline-formula><mml:math id="M93" display="inline"><mml:mrow><mml:msub><mml:mi>H</mml:mi><mml:mtext>In-CASE</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) but is equal to Eq. (4):
            <disp-formula id="Ch1.E4" content-type="numbered"><label>4</label><mml:math id="M94" display="block"><mml:mrow><mml:msub><mml:mi>H</mml:mi><mml:mtext>eff</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi>U</mml:mi><mml:mrow><mml:mi>A</mml:mi><mml:mo>,</mml:mo><mml:mi mathvariant="normal">∞</mml:mi></mml:mrow></mml:msub></mml:mrow><mml:mrow><mml:msub><mml:mi>U</mml:mi><mml:mrow><mml:mi>A</mml:mi><mml:mo>,</mml:mo><mml:mi mathvariant="normal">∞</mml:mi></mml:mrow></mml:msub><mml:mo>+</mml:mo><mml:msub><mml:mi>V</mml:mi><mml:mi>Q</mml:mi></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><mml:msub><mml:mi>H</mml:mi><mml:mtext>In-CASE</mml:mtext></mml:msub><mml:mo>.</mml:mo></mml:mrow></mml:math></disp-formula></p>
      <p id="d1e1730">However, as the droplet terminal velocity (<inline-formula><mml:math id="M95" display="inline"><mml:mrow><mml:msub><mml:mi>U</mml:mi><mml:mrow><mml:mi>A</mml:mi><mml:mo>,</mml:mo><mml:mi mathvariant="normal">∞</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>) is about 25 cm s<inline-formula><mml:math id="M96" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> and the maximum AP flow velocity (<inline-formula><mml:math id="M97" display="inline"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mi>Q</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>) considered
in the In-CASE collision chamber during the experiment is 5 mm s<inline-formula><mml:math id="M98" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> (for an AP
flow rate of 0.6 L min<inline-formula><mml:math id="M99" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>), these two heights are thus considered equal
(<inline-formula><mml:math id="M100" display="inline"><mml:mrow><mml:msub><mml:mi>H</mml:mi><mml:mtext>eff</mml:mtext></mml:msub><mml:mo>∼</mml:mo><mml:msub><mml:mi>H</mml:mi><mml:mtext>In-CASE</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>).</p>
      <p id="d1e1815">In Eq. (3), the mean AP mass concentration in the In-CASE collision
chamber is estimated from the fluorescence spectrometry analysis of the HEPA
filter though Eq. (5):
            <disp-formula id="Ch1.E5" content-type="numbered"><label>5</label><mml:math id="M101" display="block"><mml:mrow><mml:msub><mml:mi>C</mml:mi><mml:mtext>m,AP</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,tot</mml:mtext></mml:msub></mml:mrow><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi>t</mml:mi><mml:mo>×</mml:mo><mml:msub><mml:mi>Q</mml:mi><mml:mtext>In-CASE,c</mml:mtext></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>.</mml:mo></mml:mrow></mml:math></disp-formula></p>
      <p id="d1e1853"><inline-formula><mml:math id="M102" display="inline"><mml:mrow><mml:msub><mml:mi>Q</mml:mi><mml:mtext>In-CASE,c</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is the AP flow rate within the In-CASE collision chamber.</p>
</sec>
<sec id="Ch1.S3.SS2">
  <label>3.2</label><title>DMA selection – multiple charged AP's principle</title>
      <p id="d1e1874">As previously stated, the AP flow travels through a DMA to select the
particles according to their electrical mobility (<inline-formula><mml:math id="M103" display="inline"><mml:mi>Z</mml:mi></mml:math></inline-formula>), which is defined by
Eq. (6):
            <disp-formula id="Ch1.E6" content-type="numbered"><label>6</label><mml:math id="M104" display="block"><mml:mrow><mml:mi>Z</mml:mi><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mi>n</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi>e</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msub><mml:mi>C</mml:mi><mml:mi>u</mml:mi></mml:msub></mml:mrow><mml:mrow><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mn mathvariant="normal">6</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi mathvariant="italic">π</mml:mi><mml:mspace width="0.125em" linebreak="nobreak"/><mml:msub><mml:mi mathvariant="italic">η</mml:mi><mml:mtext>air</mml:mtext></mml:msub><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi>a</mml:mi></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where <inline-formula><mml:math id="M105" display="inline"><mml:mi>n</mml:mi></mml:math></inline-formula>, <inline-formula><mml:math id="M106" display="inline"><mml:mrow><mml:msub><mml:mi>C</mml:mi><mml:mi>u</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M107" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">η</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> are respectively the number of
elementary charges (<inline-formula><mml:math id="M108" display="inline"><mml:mi>e</mml:mi></mml:math></inline-formula>), the Cunningham correction coefficient and the air dynamic viscosity (expressed here in poise).</p>
      <p id="d1e1963">Thus, for an AP radius selected by the DMA, all particles with the same
<inline-formula><mml:math id="M109" display="inline"><mml:mstyle displaystyle="false"><mml:mfrac style="text"><mml:mrow><mml:mi>n</mml:mi><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msub><mml:mi>C</mml:mi><mml:mi>u</mml:mi></mml:msub></mml:mrow><mml:mi mathvariant="normal">a</mml:mi></mml:mfrac></mml:mstyle></mml:math></inline-formula> ratio are actually selected.
For example, when an AP with a radius of 50 nm is selected (single charged),
the AP radii of 75.8 nm (double charged) and 98.2 nm (triple charged) will
also be selected and progress into the In-CASE collision chamber since they
have the same electrical mobility. In this paper, “multiple charged APs”
refer to the APs with the same electrical mobility as those with
single charge selected by the DMA.</p>
      <p id="d1e1984">At the DMA's inlet, an aerodynamic impactor is placed to prevent the
heaviest APs from entering the DMA. Thus, for a given AP flow rate in the
DMA, the multiple charged APs can be impacted at the DMA's inlet and can
then be neglected at the DMA's outlet. To evaluate this case, the cut-off
radius of the impactor at the DMA's inlet must be considered (referred to as
<inline-formula><mml:math id="M110" display="inline"><mml:mrow><mml:msub><mml:mi>D</mml:mi><mml:mrow><mml:mn mathvariant="normal">50</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi mathvariant="italic">%</mml:mi></mml:mrow></mml:msub><mml:mo>/</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:math></inline-formula>). This radius is defined as the one where 50 % of the APs
are impacted. The Table 1 shows this parameter for every AP flow rate used
during the experiment and for a given selected AP radius. The double charged
AP radius with the same electrical mobility as the selected AP radius
(single charged) is also indicated – when this latter size is large enough
compared to the cut-off radius, it is assumed that there is no contribution
of the multiple charged APs in the CE measurement. This is the case for a
selected AP radius of 200 or 250 nm where the AP size distribution at the
DMA's outlet can be considered purely monodispersed.</p>
      <p id="d1e2006">However, for a selected AP radius of 50 or 150 nm, according to Table 1, the
multiple charged AP radii cannot be neglected. Different experiments were
run to perform a deconvolution of their respective contributions in the
final CE calculation. This method is presented in Appendix A.</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T1" specific-use="star"><?xmltex \currentcnt{1}?><label>Table 1</label><caption><p id="d1e2013">AP selection parameters.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="4">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="right"/>
     <oasis:colspec colnum="3" colname="col3" align="right"/>
     <oasis:colspec colnum="4" colname="col4" align="right"/>
     <oasis:thead>
       <oasis:row>
         <oasis:entry colname="col1">Selected dry AP</oasis:entry>
         <oasis:entry colname="col2">Double charged</oasis:entry>
         <oasis:entry colname="col3">AP flow rate in</oasis:entry>
         <oasis:entry colname="col4">Cut-off radius of the</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">radius by the DMA</oasis:entry>
         <oasis:entry colname="col2">dry AP radius</oasis:entry>
         <oasis:entry colname="col3">the DMA</oasis:entry>
         <oasis:entry colname="col4">impactor at the</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">(single charged)</oasis:entry>
         <oasis:entry colname="col2">with the same</oasis:entry>
         <oasis:entry colname="col3"/>
         <oasis:entry colname="col4">DMA's inlet</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1"/>
         <oasis:entry colname="col2">electrical mobility</oasis:entry>
         <oasis:entry colname="col3"/>
         <oasis:entry colname="col4">(<inline-formula><mml:math id="M111" display="inline"><mml:mrow><mml:msub><mml:mi>D</mml:mi><mml:mrow><mml:mn mathvariant="normal">50</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi mathvariant="italic">%</mml:mi></mml:mrow></mml:msub><mml:mo>/</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:math></inline-formula>)</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row>
         <oasis:entry colname="col1">50  nm</oasis:entry>
         <oasis:entry colname="col2">75.8 nm</oasis:entry>
         <oasis:entry colname="col3">0.6 L min<inline-formula><mml:math id="M112" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col4">213 nm</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">150 nm</oasis:entry>
         <oasis:entry colname="col2">253.7 nm</oasis:entry>
         <oasis:entry colname="col3">0.6 L min<inline-formula><mml:math id="M113" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col4">213 nm</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">200 nm</oasis:entry>
         <oasis:entry colname="col2">348.3 nm</oasis:entry>
         <oasis:entry colname="col3">0.6 L min<inline-formula><mml:math id="M114" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col4">213 nm</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">250 nm</oasis:entry>
         <oasis:entry colname="col2">444.3 nm</oasis:entry>
         <oasis:entry colname="col3">0.4 L min<inline-formula><mml:math id="M115" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col4">268.5 nm</oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table></table-wrap>

</sec>
<sec id="Ch1.S3.SS3">
  <label>3.3</label><title>Uncertainty evaluations</title>
<sec id="Ch1.S3.SS3.SSS1">
  <label>3.3.1</label><title>AP radius uncertainty</title>
      <p id="d1e2231">The first AP radius uncertainty is related to the AP selection by the DMA.
Nevertheless, this uncertainty has been neglected since the spectral
bandwidth of the DMA is quite small compared to the AP radius uncertainty
addressed below.</p>
      <p id="d1e2234">Indeed, the only significant AP radius uncertainty results from the
effective AP radius inside the In-CASE collision chamber due to the
hygroscopicity of the APs. For the relative humidity levels studied (71.1 %,
82.4 % or 93.5 %), the extreme relative humidity levels measured in all
experiments are considered – for 71.1 %, the minimum and maximum values
are 69.2 % and 73.4 %, respectively. As a reminder, the kappa value is
assumed from the Quérel et al. (2014) data and ranges from 0.2 to 0.27
(see Fig. 6). The low uncertainty for the AP radius is then evaluated by
considering the minimum growth factor (GroF) in Fig. 6 for the lower
level of relative humidity measured and the lower kappa value determined – respectively 69.2 % and 0.2. Similarly, for the same example (RH <inline-formula><mml:math id="M116" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 71.1 %), the high uncertainty for the AP radius is estimated by
evaluating the maximum growth factor – for the maximum level of relative
humidity observed and the maximum kappa value assumed – respectively
73.4 % and 0.27. In this example, for a dry AP radius of 50 nm selected
by the DMA, its wet radius in the In-CASE collision chamber is likely to be
58 nm (GroF <inline-formula><mml:math id="M117" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 1.16), ranging from 56.5 nm (GroF <inline-formula><mml:math id="M118" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 1.13) to 60 nm (GroF <inline-formula><mml:math id="M119" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 1.20) resulting from the respective low and high uncertainties.</p>
</sec>
<sec id="Ch1.S3.SS3.SSS2">
  <label>3.3.2</label><title>Uncertainty of the collection efficiency</title>
      <p id="d1e2273">Since the method of CE evaluation differs in the presence of multiple
charged APs, the uncertainty calculation is also different depending on the
situations. The method is described in Appendix B.</p>
      <p id="d1e2276">When there are no multiple charged APs in the AP flow, the CE is directly
estimated through Eq. (3), which can be rewritten as Eq. (7):
              <disp-formula id="Ch1.E7" content-type="numbered"><label>7</label><mml:math id="M120" display="block"><mml:mtable rowspacing="0.2ex" class="split" columnspacing="1em" displaystyle="true" columnalign="right left"><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><?xmltex \hack{\hbox\bgroup\fontsize{8.5}{8.5}\selectfont$\displaystyle}?><mml:mtext mathvariant="normal">CE</mml:mtext><mml:mo>(</mml:mo><mml:mi>a</mml:mi><mml:mo>,</mml:mo><mml:mi>A</mml:mi><mml:mo>,</mml:mo><mml:mtext>RH</mml:mtext><mml:mo>)</mml:mo><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,d</mml:mtext></mml:msub></mml:mrow><mml:mrow><mml:mi mathvariant="italic">π</mml:mi><mml:msup><mml:mfenced open="(" close=")"><mml:mrow><mml:mi>A</mml:mi><mml:mo>+</mml:mo><mml:mtext>GroF(RH)</mml:mtext><mml:mo>×</mml:mo><mml:mi>a</mml:mi></mml:mrow></mml:mfenced><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mo>×</mml:mo><mml:msub><mml:mi>N</mml:mi><mml:mtext>d</mml:mtext></mml:msub><mml:mo>×</mml:mo><mml:msub><mml:mi>H</mml:mi><mml:mtext>eff</mml:mtext></mml:msub><mml:mo>×</mml:mo><mml:msub><mml:mi>C</mml:mi><mml:mtext>m,AP</mml:mtext></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><?xmltex \hack{$\egroup}?></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:mo>≈</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,d</mml:mtext></mml:msub></mml:mrow><mml:mrow><mml:mi mathvariant="italic">π</mml:mi><mml:msup><mml:mi>A</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mo>×</mml:mo><mml:msub><mml:mi>N</mml:mi><mml:mtext>d</mml:mtext></mml:msub><mml:mo>×</mml:mo><mml:msub><mml:mi>H</mml:mi><mml:mtext>eff</mml:mtext></mml:msub><mml:mo>×</mml:mo><mml:msub><mml:mi>C</mml:mi><mml:mtext>m,AP</mml:mtext></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><mml:mo>,</mml:mo></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula>
            where <inline-formula><mml:math id="M121" display="inline"><mml:mrow><mml:msub><mml:mi>N</mml:mi><mml:mtext>d</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is the number of injected droplets during the experiment. The
relative CE uncertainty (<inline-formula><mml:math id="M122" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mtext>CE</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) is then evaluated according to Lira
(2002) and summarised by Eq. (8),
              <disp-formula id="Ch1.E8" content-type="numbered"><label>8</label><mml:math id="M123" display="block"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mtext>CE</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:msqrt><mml:mrow><mml:msubsup><mml:mi>u</mml:mi><mml:mi>A</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup><mml:mo>+</mml:mo><mml:msubsup><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>H</mml:mi><mml:mtext>eff</mml:mtext></mml:msub></mml:mrow><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup><mml:mo>+</mml:mo><mml:msubsup><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>N</mml:mi><mml:mtext>d</mml:mtext></mml:msub></mml:mrow><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup><mml:mo>+</mml:mo><mml:msubsup><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,d</mml:mtext></mml:msub></mml:mrow><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup><mml:mo>+</mml:mo><mml:msubsup><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>C</mml:mi><mml:mtext>m,AP</mml:mtext></mml:msub></mml:mrow><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup></mml:mrow></mml:msqrt><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
            with the following.
<list list-type="bullet"><list-item>
      <p id="d1e2501">The relative uncertainty related to the droplet radius measurement (<inline-formula><mml:math id="M124" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mi>A</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>),
which is the ratio between the standard deviation and the mean droplet
radius on 200 pictures obtained by optical shadowgraphy. This relative
uncertainty is about 1 %.</p></list-item><list-item>
      <p id="d1e2516">The relative uncertainty of the effective height of interaction between
droplets and APs (<inline-formula><mml:math id="M125" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>H</mml:mi><mml:mtext>eff</mml:mtext></mml:msub></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>), which is 4 %. Indeed, it has been
evaluated that a maximum of 4 cm is required to assure a good AP mixing at the
injection in the collision chamber of 1 m height (<inline-formula><mml:math id="M126" display="inline"><mml:mrow><mml:msub><mml:mi>H</mml:mi><mml:mtext>In-CASE</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>).</p></list-item><list-item>
      <p id="d1e2546">The relative uncertainty of the number of droplets (<inline-formula><mml:math id="M127" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>N</mml:mi><mml:mtext>d</mml:mtext></mml:msub></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>) which can
be correlated to the droplet number effectively impacted on the droplet
impaction cup. This relative uncertainty was evaluated during the validation
of AP and droplet train separation (“Validation” in Sect. 2.2.2) and is about 2 %.</p></list-item><list-item>
      <p id="d1e2565">The relative uncertainty of the detected AP mass in the droplet impaction
cup (<inline-formula><mml:math id="M128" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,d</mml:mtext></mml:msub></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>), which takes into account the relative uncertainty
related to the spectrometry analysis (<inline-formula><mml:math id="M129" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mtext>fluorimeter</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) and the one caused
by the dilution (<inline-formula><mml:math id="M130" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mtext>dilution</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>), Eq. (9). Indeed, at the end of an
experiment the water contained in the droplet impaction cup is dried and the
residual AP mass is then dissolved in 2 mL volume of ammonia water.<disp-formula id="Ch1.E9" content-type="numbered"><label>9</label><mml:math id="M131" display="block"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,d</mml:mtext></mml:msub></mml:mrow></mml:msub><mml:mo>=</mml:mo><mml:msqrt><mml:mrow><mml:msubsup><mml:mi>u</mml:mi><mml:mi mathvariant="normal">fluorimeter</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup><mml:mo>+</mml:mo><mml:msubsup><mml:mi>u</mml:mi><mml:mi mathvariant="normal">dilution</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup></mml:mrow></mml:msqrt><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>where <inline-formula><mml:math id="M132" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mtext>dilution</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is estimated at 1 % while <inline-formula><mml:math id="M133" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mtext>fluorimeter</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is the main source of
uncertainty. In fact, when the mass of AP collected by the droplet is close
to the detection limit of the fluorimeter (about 10<inline-formula><mml:math id="M134" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">15</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> kg in the
droplet sample volume analysed), <inline-formula><mml:math id="M135" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mtext>fluorimeter</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is up to 30 %.</p></list-item><list-item>
      <p id="d1e2689">The relative uncertainty of the mean AP mass concentration in the In-CASE
collision chamber (<inline-formula><mml:math id="M136" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>C</mml:mi><mml:mtext>m,AP</mml:mtext></mml:msub></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>) which can be evaluated, according to
Eq. (5), by Eq. (10):<disp-formula id="Ch1.E10" content-type="numbered"><label>10</label><mml:math id="M137" display="block"><mml:mtable columnspacing="1em" rowspacing="0.2ex" class="split" displaystyle="true" columnalign="right left"><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>C</mml:mi><mml:mtext>m,AP</mml:mtext></mml:msub></mml:mrow></mml:msub><mml:mo>=</mml:mo><mml:msqrt><mml:mrow><mml:msubsup><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,tot</mml:mtext></mml:msub></mml:mrow><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup><mml:mo>+</mml:mo><mml:msubsup><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>Q</mml:mi><mml:mtext>In-CASE,c</mml:mtext></mml:msub></mml:mrow><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup><mml:mo>+</mml:mo><mml:msubsup><mml:mi>u</mml:mi><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi>t</mml:mi></mml:mrow><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup></mml:mrow></mml:msqrt></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:mo>≈</mml:mo><mml:msqrt><mml:mrow><mml:msubsup><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,tot</mml:mtext></mml:msub></mml:mrow><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup><mml:mo>+</mml:mo><mml:msubsup><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>Q</mml:mi><mml:mtext>In-CASE,c</mml:mtext></mml:msub></mml:mrow><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup></mml:mrow></mml:msqrt></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,tot</mml:mtext></mml:msub></mml:mrow></mml:msub><mml:mo>=</mml:mo><mml:msqrt><mml:mrow><mml:msubsup><mml:mi>u</mml:mi><mml:mtext>fluorimeter</mml:mtext><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup><mml:mo>+</mml:mo><mml:msubsup><mml:mi>u</mml:mi><mml:mtext>dilution</mml:mtext><mml:mn mathvariant="normal">2</mml:mn></mml:msubsup></mml:mrow></mml:msqrt><mml:mo>,</mml:mo></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula>where the relative uncertainty of the detected AP mass on the HEPA filter
(<inline-formula><mml:math id="M138" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,tot</mml:mtext></mml:msub></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>) depends on the one on the fluorimeter (<inline-formula><mml:math id="M139" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mtext>fluorimeter</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>)
and the one on the dilution (<inline-formula><mml:math id="M140" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mtext>dilution</mml:mtext></mml:msub><mml:mo>∼</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:math></inline-formula> %). In fact, the
spectrometry analysis is performed by diluting the AP mass on the HEPA
filter in a 100 mL ammonia water solution at the end of an experiment. The
relative uncertainty of the AP flow rate in the In-CASE collision chamber
(<inline-formula><mml:math id="M141" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mrow><mml:msub><mml:mi>Q</mml:mi><mml:mtext>In-CASE,c</mml:mtext></mml:msub></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>) is given by the data sheet of the constructor – about
1 %. Note that the relative uncertainty on the experiment time
(<inline-formula><mml:math id="M142" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi>t</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>) is neglected since the error is approximately 1 s
on an experiment that can last more than 5 h.</p></list-item></list></p>
</sec>
</sec>
</sec>
<?pagebreak page6954?><sec id="Ch1.S4">
  <label>4</label><title>Results and discussions</title>
<sec id="Ch1.S4.SS1">
  <label>4.1</label><?xmltex \opttitle{Extension of the D\'{e}p\'{e}e et al.~(2019) model}?><title>Extension of the Dépée et al. (2019) model</title>
      <p id="d1e2922">In all experiments, the droplet charge is <inline-formula><mml:math id="M143" display="inline"><mml:mrow><mml:mn mathvariant="normal">0</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">600</mml:mn></mml:mrow></mml:math></inline-formula> elementary charges
with a radius of about 50 <inline-formula><mml:math id="M144" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m. Since the AP charge distribution is
similar to a Boltzmann distribution, an AP charge of more than 5 elementary
charges is thus highly unlikely in the radius range considered in the
experiments. Moreover, Dépée et al. (2019) numerically evaluated the
contribution of the electrostatic forces on the CE for a droplet of 50 <inline-formula><mml:math id="M145" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m radius with <inline-formula><mml:math id="M146" display="inline"><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1000</mml:mn></mml:mrow></mml:math></inline-formula> elementary charges and 5 elementary charges on the AP.
For these extreme values, they calculate an increase in the CE due to the
electrostatic forces by 42 % and 22 % for an AP radius of 50 and
300 nm, respectively. Close to these two AP radii, a rise of the CE by a
factor of 3 and 4, respectively, is observed when the relative humidity goes
from <inline-formula><mml:math id="M147" display="inline"><mml:mrow><mml:mn mathvariant="normal">93.5</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">0.9</mml:mn></mml:mrow></mml:math></inline-formula> % to <inline-formula><mml:math id="M148" display="inline"><mml:mrow><mml:mn mathvariant="normal">71.1</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">1.3</mml:mn></mml:mrow></mml:math></inline-formula> % (Fig. 10).
Consequently, it is assumed that the contribution of the thermophoresis and
the diffusiophoresis is of first order in the<?pagebreak page6955?> measurements and the
electrostatic forces can be neglected in the observed increase in CE.</p>
      <p id="d1e2988">To extend the Dépée et al. (2019) model for the thermophoretic
(<inline-formula><mml:math id="M149" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="bold-italic">F</mml:mi><mml:mi mathvariant="bold">th</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>) and diffusiophoretic forces
(<inline-formula><mml:math id="M150" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="bold-italic">F</mml:mi><mml:mi mathvariant="bold">df</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>), the resulting velocity at the AP location
(<inline-formula><mml:math id="M151" display="inline"><mml:mrow><mml:msubsup><mml:mi mathvariant="bold-italic">U</mml:mi><mml:mrow><mml:mi>f</mml:mi><mml:mi mathvariant="normal">@</mml:mi><mml:mi>p</mml:mi></mml:mrow><mml:mo>∗</mml:mo></mml:msubsup></mml:mrow></mml:math></inline-formula>) given by the authors (in Eq. 6) is
replaced by  Eq. (11):
            <disp-formula id="Ch1.E11" content-type="numbered"><label>11</label><mml:math id="M152" display="block"><mml:mrow><?xmltex \hack{\hbox\bgroup\fontsize{9.2}{9.2}\selectfont$\displaystyle}?><mml:msup><mml:msub><mml:mi mathvariant="bold-italic">U</mml:mi><mml:mrow><mml:mi>f</mml:mi><mml:mi mathvariant="normal">@</mml:mi><mml:mtext>AP</mml:mtext></mml:mrow></mml:msub><mml:mo>∗</mml:mo></mml:msup><mml:mo>(</mml:mo><mml:mi>t</mml:mi><mml:mo>)</mml:mo><mml:mo>=</mml:mo><mml:msub><mml:mi mathvariant="bold-italic">U</mml:mi><mml:mrow><mml:mi>f</mml:mi><mml:mi mathvariant="normal">@</mml:mi><mml:mtext>AP</mml:mtext></mml:mrow></mml:msub><mml:mo>(</mml:mo><mml:mi>t</mml:mi><mml:mo>)</mml:mo><mml:mo>+</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>AP</mml:mtext></mml:msub></mml:mrow><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP</mml:mtext></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><mml:mfenced close=")" open="("><mml:mrow><mml:msub><mml:mi mathvariant="bold-italic">F</mml:mi><mml:mtext>buoy</mml:mtext></mml:msub><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="bold-italic">F</mml:mi><mml:mtext>df</mml:mtext></mml:msub><mml:mo>+</mml:mo><mml:msub><mml:mi mathvariant="bold-italic">F</mml:mi><mml:mtext>th</mml:mtext></mml:msub></mml:mrow></mml:mfenced><?xmltex \hack{$\egroup}?><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where <inline-formula><mml:math id="M153" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="bold-italic">F</mml:mi><mml:mtext>buoy</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is the buoyancy force, <inline-formula><mml:math id="M154" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="bold-italic">U</mml:mi><mml:mrow><mml:mi>f</mml:mi><mml:mi mathvariant="normal">@</mml:mi><mml:mtext>AP</mml:mtext></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula> is the fluid velocity at
the AP location, <inline-formula><mml:math id="M155" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">τ</mml:mi><mml:mtext>AP</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is the AP relaxation time and <inline-formula><mml:math id="M156" display="inline"><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> is the AP
mass. The thermophoresis and the diffusiophoresis which are given by Brock
(1962) and Waldmann and Schmitt (1966), respectively, are summarised in
Eq. (12):
            <disp-formula id="Ch1.E12" content-type="numbered"><label>12</label><mml:math id="M157" display="block"><mml:mrow><mml:mfenced open="{" close=""><mml:mtable rowspacing="11.381102pt 11.381102pt" class="array" columnalign="left"><mml:mtr><mml:mtd><mml:mrow><mml:msub><mml:mi mathvariant="bold-italic">F</mml:mi><mml:mi mathvariant="bold">df</mml:mi></mml:msub><mml:mo>=</mml:mo><mml:mo>-</mml:mo><mml:mn mathvariant="normal">6</mml:mn><mml:mi mathvariant="italic">π</mml:mi><mml:msub><mml:mi mathvariant="italic">η</mml:mi><mml:mtext>air</mml:mtext></mml:msub><mml:mi>a</mml:mi><mml:mstyle displaystyle="false"><mml:mstyle displaystyle="false"><mml:mfrac style="text"><mml:mrow><mml:mn mathvariant="normal">0</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">74</mml:mn><mml:msub><mml:mi>D</mml:mi><mml:mtext>v</mml:mtext></mml:msub><mml:msub><mml:mi>M</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow><mml:mrow><mml:msub><mml:mi>C</mml:mi><mml:mi>u</mml:mi></mml:msub><mml:msub><mml:mi>M</mml:mi><mml:mtext>water</mml:mtext></mml:msub><mml:msub><mml:mi mathvariant="italic">ρ</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow></mml:mfrac></mml:mstyle></mml:mstyle><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mo>×</mml:mo><mml:mstyle displaystyle="false"><mml:mstyle displaystyle="false"><mml:mfrac style="text"><mml:mrow><mml:mover><mml:mover accent="true" class="overbrace"><mml:mrow><mml:mo>(</mml:mo><mml:msub><mml:mi mathvariant="italic">ρ</mml:mi><mml:mrow><mml:mi>v</mml:mi><mml:mo>,</mml:mo><mml:mtext>air</mml:mtext></mml:mrow></mml:msub><mml:mo>-</mml:mo><mml:msub><mml:mi mathvariant="italic">ρ</mml:mi><mml:mrow><mml:mi>v</mml:mi><mml:mo>,</mml:mo><mml:mi>s</mml:mi></mml:mrow></mml:msub><mml:mo>)</mml:mo><mml:msub><mml:mi>f</mml:mi><mml:mtext>v</mml:mtext></mml:msub></mml:mrow><mml:mo mathvariant="normal">︷</mml:mo></mml:mover><mml:mrow><mml:mo>(</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:mo>)</mml:mo></mml:mrow></mml:mover></mml:mrow><mml:mrow><mml:mi>A</mml:mi><mml:msup><mml:mi>r</mml:mi><mml:mrow><mml:mo>∗</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:mfrac></mml:mstyle></mml:mstyle><mml:msub><mml:mi mathvariant="bold-italic">u</mml:mi><mml:mi mathvariant="normal">r</mml:mi></mml:msub></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:msub><mml:mi mathvariant="bold-italic">F</mml:mi><mml:mi mathvariant="bold">th</mml:mi></mml:msub><mml:mo>=</mml:mo><mml:mo>-</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mn mathvariant="normal">12</mml:mn><mml:mi mathvariant="italic">π</mml:mi><mml:msub><mml:mi mathvariant="italic">η</mml:mi><mml:mtext>air</mml:mtext></mml:msub><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:mn mathvariant="normal">5</mml:mn><mml:msub><mml:mi>P</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow></mml:mfrac></mml:mstyle><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mfenced close=")" open="("><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mtext>air</mml:mtext></mml:msub><mml:mo>+</mml:mo><mml:mn mathvariant="normal">2</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">5</mml:mn><mml:msub><mml:mi>k</mml:mi><mml:mtext>AP</mml:mtext></mml:msub><mml:mi>K</mml:mi><mml:mi>n</mml:mi></mml:mrow></mml:mfenced><mml:msub><mml:mi>k</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow><mml:mrow><mml:mfenced close=")" open="("><mml:mrow><mml:mn mathvariant="normal">1</mml:mn><mml:mo>+</mml:mo><mml:mn mathvariant="normal">3</mml:mn><mml:mi>K</mml:mi><mml:mi>n</mml:mi></mml:mrow></mml:mfenced><mml:mfenced open="(" close=")"><mml:mrow><mml:mn mathvariant="normal">2</mml:mn><mml:msub><mml:mi>k</mml:mi><mml:mtext>air</mml:mtext></mml:msub><mml:mo>+</mml:mo><mml:msub><mml:mi>k</mml:mi><mml:mtext>AP</mml:mtext></mml:msub><mml:mo>+</mml:mo><mml:mn mathvariant="normal">5</mml:mn><mml:msub><mml:mi>k</mml:mi><mml:mtext>AP</mml:mtext></mml:msub><mml:mi>K</mml:mi><mml:mi>n</mml:mi></mml:mrow></mml:mfenced></mml:mrow></mml:mfrac></mml:mstyle></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><?xmltex \hack{\hspace*{8mm}}?><mml:mo>×</mml:mo><mml:munder><mml:munder class="underbrace"><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:mo>(</mml:mo><mml:msub><mml:mi>T</mml:mi><mml:mtext>air</mml:mtext></mml:msub><mml:mo>-</mml:mo><mml:msub><mml:mi>T</mml:mi><mml:mrow><mml:mi>d</mml:mi><mml:mo>,</mml:mo><mml:mi>s</mml:mi></mml:mrow></mml:msub><mml:mo>)</mml:mo><mml:msub><mml:mi>f</mml:mi><mml:mtext>h</mml:mtext></mml:msub></mml:mrow><mml:mrow><mml:mi>A</mml:mi><mml:msup><mml:mi>r</mml:mi><mml:mrow><mml:mo>∗</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:mfrac></mml:mstyle><mml:mo mathvariant="normal">︸</mml:mo></mml:munder><mml:mrow><mml:mo>(</mml:mo><mml:mn mathvariant="normal">2</mml:mn><mml:mo>)</mml:mo></mml:mrow></mml:munder><mml:msub><mml:mi mathvariant="bold-italic">u</mml:mi><mml:mi mathvariant="normal">r</mml:mi></mml:msub><mml:mo>,</mml:mo></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:mfenced></mml:mrow></mml:math></disp-formula>
          with <inline-formula><mml:math id="M158" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="bold-italic">u</mml:mi><mml:mi mathvariant="normal">r</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula> the unit vector in the radial direction
from the droplet centre to the AP centre, <inline-formula><mml:math id="M159" display="inline"><mml:mrow><mml:msup><mml:mi>r</mml:mi><mml:mo>∗</mml:mo></mml:msup></mml:mrow></mml:math></inline-formula> the distance between
the AP and droplet centres normalised by the droplet radius <inline-formula><mml:math id="M160" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>, <inline-formula><mml:math id="M161" display="inline"><mml:mrow><mml:msub><mml:mi>D</mml:mi><mml:mtext>v</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> the diffusivity of vapour, <inline-formula><mml:math id="M162" display="inline"><mml:mrow><mml:mi>K</mml:mi><mml:mi>n</mml:mi></mml:mrow></mml:math></inline-formula> the Knudsen number, <inline-formula><mml:math id="M163" display="inline"><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> and
<inline-formula><mml:math id="M164" display="inline"><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mtext>water</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> the respective air and water molar masses, and <inline-formula><mml:math id="M165" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> and
<inline-formula><mml:math id="M166" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mtext>AP</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> the respective air and AP thermal conductivities. Note that the
thermal conductivity of the sodium fluorescein salt is considered for
<inline-formula><mml:math id="M167" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mtext>AP</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> – equal to 0.43 m kg s<inline-formula><mml:math id="M168" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> K<inline-formula><mml:math id="M169" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> (Al-Azzawi and Owen, 1984).</p>
      <p id="d1e3603">In Eq. (12), the terms (1) and (2) represent the gradient of vapour density
and the thermal gradient in the air, respectively. These two gradients are
computed under the assumption that the temperature and vapour density
profiles are spherically symmetric around the droplet (Wang et al., 1978).
Because the droplet is falling in the air, <inline-formula><mml:math id="M170" display="inline"><mml:mrow><mml:msub><mml:mi>f</mml:mi><mml:mtext>v</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M171" display="inline"><mml:mrow><mml:msub><mml:mi>f</mml:mi><mml:mtext>h</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> – which are
the ventilation coefficients for the vapour and the heat respectively (Beard
and Pruppacher, 1971) – correct the gradients since the profiles are
actually disturbed by the airflow.</p>

<?xmltex \floatpos{p}?><table-wrap id="Ch1.T2" specific-use="star"><?xmltex \currentcnt{2}?><label>Table 2</label><caption><p id="d1e3632">Key features of the In-CASE setup.</p></caption><oasis:table frame="topbot"><?xmltex \begin{scaleboxenv}{.87}[.87]?><oasis:tgroup cols="2">
     <oasis:colspec colnum="1" colname="col1" align="justify" colwidth="260pt"/>
     <oasis:colspec colnum="2" colname="col2" align="justify" colwidth="260pt"/>
     <oasis:thead>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Feature</oasis:entry>
         <oasis:entry colname="col2">Numerical value</oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row rowsep="1">
         <oasis:entry namest="col1" nameend="col2" align="left">Collision chamber's parameters </oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Height of the collision chamber (<inline-formula><mml:math id="M172" display="inline"><mml:mrow><mml:msub><mml:mi>H</mml:mi><mml:mtext>In-CASE</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2">1 m</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Distance between droplet injection and AP injection</oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M173" display="inline"><mml:mrow><mml:mo>≈</mml:mo><mml:mn mathvariant="normal">10</mml:mn></mml:mrow></mml:math></inline-formula> cm</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Diameter of the collision chamber</oasis:entry>
         <oasis:entry colname="col2">5 cm</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Impaction cup diameter</oasis:entry>
         <oasis:entry colname="col2">2.5 cm</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">AP flow rate in the collision chamber (<inline-formula><mml:math id="M174" display="inline"><mml:mrow><mml:msub><mml:mi>Q</mml:mi><mml:mtext>In-CASE, c</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2">0.4 or 0.6 L min<inline-formula><mml:math id="M175" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> (following the selected AP radius)</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Flow velocity in the collision chamber (<inline-formula><mml:math id="M176" display="inline"><mml:mrow><mml:msub><mml:mi>V</mml:mi><mml:mi>Q</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2">3.4 or 5.1 mm s<inline-formula><mml:math id="M177" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> (following the selected AP radius)</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Flow rate of the upward Argon at the inlet of AP/droplet separator</oasis:entry>
         <oasis:entry colname="col2">0.4 L min<inline-formula><mml:math id="M178" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Flow rate of the upward Argon in the impaction cup</oasis:entry>
         <oasis:entry colname="col2">1.4 cm s<inline-formula><mml:math id="M179" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">AP and Argon flow rate at the outlet of In-CASE chamber (toward <?xmltex \hack{\hfill\break}?>the HEPA filter)</oasis:entry>
         <oasis:entry colname="col2">0.8 or 1 L min<inline-formula><mml:math id="M180" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> (following the selected AP radius)</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Air pressure in the collision chamber (<inline-formula><mml:math id="M181" display="inline"><mml:mrow><mml:msub><mml:mi>P</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2">1 atm</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Temperature in the collision chamber (<inline-formula><mml:math id="M182" display="inline"><mml:mrow><mml:msub><mml:mi>T</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M183" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.58</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">0.50</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M184" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Relative humidity in the collision chamber (RH)</oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M185" display="inline"><mml:mrow><mml:mn mathvariant="normal">71.1</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">1.3</mml:mn></mml:mrow></mml:math></inline-formula> %, <inline-formula><mml:math id="M186" display="inline"><mml:mrow><mml:mn mathvariant="normal">82.4</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">1.4</mml:mn></mml:mrow></mml:math></inline-formula> % or <inline-formula><mml:math id="M187" display="inline"><mml:mrow><mml:mn mathvariant="normal">93.5</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">0.9</mml:mn></mml:mrow></mml:math></inline-formula> %</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Duration of experiments (<inline-formula><mml:math id="M188" display="inline"><mml:mrow><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi>t</mml:mi></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2">From 3 to 6 h (related to the expected AP mass in droplets)</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry namest="col1" nameend="col2" align="left">AP's parameters </oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Selected dry AP radius during experiment (<inline-formula><mml:math id="M189" display="inline"><mml:mi>a</mml:mi></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2">50, 150, 200 or 250 nm</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Dry AP radii considered for the CE evaluation (AP charge at the <?xmltex \hack{\hfill\break}?>DMA's outlet)</oasis:entry>
         <oasis:entry colname="col2">50 (single charged), 75.8 (double charged), 98.2 (triple charged), 150 (single charged), 200 (single charged) and 250 nm (single or double charged)</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Growth factor of the APs (GroF)</oasis:entry>
         <oasis:entry colname="col2">1.16, 1.27 or 1.57</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Density of sodium fluorescein (<inline-formula><mml:math id="M190" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">ρ</mml:mi><mml:mtext>fluorescein</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2">1580 kg m<inline-formula><mml:math id="M191" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Density of the wet APs (<inline-formula><mml:math id="M192" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">ρ</mml:mi><mml:mtext>AP</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2">1372, 1283 or 1150 kg m<inline-formula><mml:math id="M193" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">AP terminal velocity</oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M194" display="inline"><mml:mrow><mml:mo>≤</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> cm s<inline-formula><mml:math id="M195" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> (equal to <inline-formula><mml:math id="M196" display="inline"><mml:mrow><mml:mn mathvariant="normal">8</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">4</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula> cm s<inline-formula><mml:math id="M197" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> for the larger selected dry AP radius 250 nm)</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">AP residence time in the collision chamber</oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M198" display="inline"><mml:mrow><mml:mo>≈</mml:mo><mml:mn mathvariant="normal">200</mml:mn></mml:mrow></mml:math></inline-formula> or 300 s (following the selected AP radius)</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Total AP concentration (single and multiple charged at the <?xmltex \hack{\hfill\break}?>DMA's outlet)</oasis:entry>
         <oasis:entry colname="col2">From <inline-formula><mml:math id="M199" display="inline"><mml:mrow><mml:mn mathvariant="normal">5</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:mrow></mml:math></inline-formula> cm<inline-formula><mml:math id="M200" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> (for a selected dry AP radius of 50 nm) to <inline-formula><mml:math id="M201" display="inline"><mml:mrow><mml:mn mathvariant="normal">6</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:mrow></mml:math></inline-formula> cm<inline-formula><mml:math id="M202" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula> (for a selected dry AP radius of 250 nm)</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">AP charge (<inline-formula><mml:math id="M203" display="inline"><mml:mi>q</mml:mi></mml:math></inline-formula>) distribution</oasis:entry>
         <oasis:entry colname="col2">Similar to Boltzmann distribution</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry namest="col1" nameend="col2" align="left">Droplet's parameters </oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Droplet radius (<inline-formula><mml:math id="M204" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M205" display="inline"><mml:mrow><mml:mn mathvariant="normal">49.6</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">1.3</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M206" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Droplet generation frequency (<inline-formula><mml:math id="M207" display="inline"><mml:mrow><mml:msub><mml:mi>F</mml:mi><mml:mtext>d</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2">25 Hz</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Droplet terminal velocity (<inline-formula><mml:math id="M208" display="inline"><mml:mrow><mml:msub><mml:mi>U</mml:mi><mml:mrow><mml:mi>A</mml:mi><mml:mo>,</mml:mo><mml:mi mathvariant="normal">∞</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M209" display="inline"><mml:mrow><mml:mo>≈</mml:mo><mml:mn mathvariant="normal">25</mml:mn></mml:mrow></mml:math></inline-formula> cm s<inline-formula><mml:math id="M210" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Number of injected droplets during experiments (<inline-formula><mml:math id="M211" display="inline"><mml:mrow><mml:msub><mml:mi>N</mml:mi><mml:mtext>d</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2">From 270 000 to 540 000 (related to the expected AP mass in droplets)</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Observed distance between two successive droplets</oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M212" display="inline"><mml:mrow><mml:mo>≈</mml:mo><mml:mn mathvariant="normal">9</mml:mn></mml:mrow></mml:math></inline-formula> mm <inline-formula><mml:math id="M213" display="inline"><mml:mo>≈</mml:mo></mml:math></inline-formula> 180 droplet radii</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Droplet residence time in the collision chamber</oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M214" display="inline"><mml:mrow><mml:mo>≈</mml:mo><mml:mn mathvariant="normal">4</mml:mn></mml:mrow></mml:math></inline-formula> s</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Droplet charge before neutralisation (<inline-formula><mml:math id="M215" display="inline"><mml:mi>Q</mml:mi></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M216" display="inline"><mml:mo>-</mml:mo></mml:math></inline-formula>8400 elementary charges</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Droplet charge after neutralisation (<inline-formula><mml:math id="M217" display="inline"><mml:mi>Q</mml:mi></mml:math></inline-formula>)</oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M218" display="inline"><mml:mrow><mml:mn mathvariant="normal">0</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">600</mml:mn></mml:mrow></mml:math></inline-formula> elementary charges</oasis:entry>
       </oasis:row>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1">Droplet evaporation between the injection and the end of <?xmltex \hack{\hfill\break}?>the collision chamber</oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M219" display="inline"><mml:mrow><mml:mo>≈</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:math></inline-formula> %,  <inline-formula><mml:math id="M220" display="inline"><mml:mrow><mml:mo>≈</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:math></inline-formula> % or <inline-formula><mml:math id="M221" display="inline"><mml:mrow><mml:mo>≈</mml:mo><mml:mn mathvariant="normal">0.6</mml:mn></mml:mrow></mml:math></inline-formula> % for the three levels of relative humidity <?xmltex \hack{\hfill\break}?>considered</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1">Sodium chloride concentration in the pure water</oasis:entry>
         <oasis:entry colname="col2">3.3 g L<inline-formula><mml:math id="M222" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula></oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup><?xmltex \end{scaleboxenv}?></oasis:table></table-wrap>

</sec>
<sec id="Ch1.S4.SS2">
  <label>4.2</label><title>Collection efficiency measurements and analysis</title>
      <p id="d1e4533">In Fig. 10, the CEs are presented for the three levels of relative
humidity studied – 71.1 %, 82.4 % and 93.5 % – and six dry AP radii ranging
from 50 to 250 nm. The numerical values are presented in Table 3. As a
reminder, all experiments were conducted with an air temperature of <inline-formula><mml:math id="M223" display="inline"><mml:mrow><mml:mn mathvariant="normal">0.58</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">0.50</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M224" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C at the atmospheric pressure, the AP charge
distribution is similar to a Boltzmann distribution and the droplet charge
is <inline-formula><mml:math id="M225" display="inline"><mml:mrow><mml:mn mathvariant="normal">0</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">600</mml:mn></mml:mrow></mml:math></inline-formula> elementary charges. The droplet radius is <inline-formula><mml:math id="M226" display="inline"><mml:mrow><mml:mn mathvariant="normal">49.6</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">1.3</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M227" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m. The key features of the experiments are summarised in Table 2. The
measurements are compared to computed efficiencies using the models
described in Wang et al. (1978) (dashed lines) as well as the extended
version of Dépée et al. (2019) (solid lines). Note that the
experimental conditions vary a little for the CE measurements at a given
relative humidity level. For the modelling, air temperature and droplet
radius are then the mean values of the three levels of relative humidity – <inline-formula><mml:math id="M228" display="inline"><mml:mrow><mml:msub><mml:mi>T</mml:mi><mml:mtext>air</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.26</mml:mn></mml:mrow></mml:math></inline-formula>, 0.27 and 1.2 <inline-formula><mml:math id="M229" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C – <inline-formula><mml:math id="M230" display="inline"><mml:mrow><mml:mi>A</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">49.3</mml:mn></mml:mrow></mml:math></inline-formula>, 50.8 and
48.8 <inline-formula><mml:math id="M231" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m – from the lowest to the highest, respectively. For RH <inline-formula><mml:math id="M232" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 100 %, these parameters are those from Table 2.</p>

<?xmltex \floatpos{t}?><table-wrap id="Ch1.T3" specific-use="star"><?xmltex \currentcnt{3}?><label>Table 3</label><caption><p id="d1e4644">CE measurements for the three levels of relative humidity (RH) and
the wet AP radii (<inline-formula><mml:math id="M233" display="inline"><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mtext>wet</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>). The droplet radius is <inline-formula><mml:math id="M234" display="inline"><mml:mrow><mml:mn mathvariant="normal">49.6</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">1.3</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M235" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m.</p></caption><oasis:table frame="topbot"><oasis:tgroup cols="6">
     <oasis:colspec colnum="1" colname="col1" align="left"/>
     <oasis:colspec colnum="2" colname="col2" align="right" colsep="1"/>
     <oasis:colspec colnum="3" colname="col3" align="right"/>
     <oasis:colspec colnum="4" colname="col4" align="right" colsep="1"/>
     <oasis:colspec colnum="5" colname="col5" align="right"/>
     <oasis:colspec colnum="6" colname="col6" align="right"/>
     <oasis:thead>
       <oasis:row rowsep="1">
         <oasis:entry namest="col1" nameend="col2" align="center" colsep="1">RH <inline-formula><mml:math id="M236" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 3.5 % </oasis:entry>
         <oasis:entry namest="col3" nameend="col4" align="center" colsep="1">RH <inline-formula><mml:math id="M237" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 82.4 % </oasis:entry>
         <oasis:entry namest="col5" nameend="col6" align="center">RH <inline-formula><mml:math id="M238" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 71.1 % </oasis:entry>
       </oasis:row>
     </oasis:thead>
     <oasis:tbody>
       <oasis:row rowsep="1">
         <oasis:entry colname="col1"><inline-formula><mml:math id="M239" display="inline"><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mtext>wet</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> (nm)</oasis:entry>
         <oasis:entry colname="col2">CE (–)</oasis:entry>
         <oasis:entry colname="col3"><inline-formula><mml:math id="M240" display="inline"><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mtext>wet</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> (nm)</oasis:entry>
         <oasis:entry colname="col4">CE (–)</oasis:entry>
         <oasis:entry colname="col5"><inline-formula><mml:math id="M241" display="inline"><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mtext>wet</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> (nm)</oasis:entry>
         <oasis:entry colname="col6">CE (–)</oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M242" display="inline"><mml:mn mathvariant="normal">79</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M243" display="inline"><mml:mrow><mml:mn mathvariant="normal">3.92</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col3"><inline-formula><mml:math id="M244" display="inline"><mml:mn mathvariant="normal">64</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M245" display="inline"><mml:mrow><mml:mn mathvariant="normal">7.15</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5"><inline-formula><mml:math id="M246" display="inline"><mml:mn mathvariant="normal">58</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col6"><inline-formula><mml:math id="M247" display="inline"><mml:mrow><mml:mn mathvariant="normal">1.18</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M248" display="inline"><mml:mn mathvariant="normal">119</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M249" display="inline"><mml:mrow><mml:mn mathvariant="normal">2.98</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col3"><inline-formula><mml:math id="M250" display="inline"><mml:mn mathvariant="normal">96</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M251" display="inline"><mml:mrow><mml:mn mathvariant="normal">5.52</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5"><inline-formula><mml:math id="M252" display="inline"><mml:mn mathvariant="normal">88</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col6"><inline-formula><mml:math id="M253" display="inline"><mml:mrow><mml:mn mathvariant="normal">1.12</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M254" display="inline"><mml:mn mathvariant="normal">154</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M255" display="inline"><mml:mrow><mml:mn mathvariant="normal">3.17</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col3"><inline-formula><mml:math id="M256" display="inline"><mml:mn mathvariant="normal">125</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M257" display="inline"><mml:mrow><mml:mn mathvariant="normal">5.16</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5"><inline-formula><mml:math id="M258" display="inline"><mml:mn mathvariant="normal">114</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col6"><inline-formula><mml:math id="M259" display="inline"><mml:mrow><mml:mn mathvariant="normal">8.94</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M260" display="inline"><mml:mn mathvariant="normal">235</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M261" display="inline"><mml:mrow><mml:mn mathvariant="normal">2.48</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col3"><inline-formula><mml:math id="M262" display="inline"><mml:mn mathvariant="normal">191</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M263" display="inline"><mml:mrow><mml:mn mathvariant="normal">5.20</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5"><inline-formula><mml:math id="M264" display="inline"><mml:mn mathvariant="normal">174</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col6"><inline-formula><mml:math id="M265" display="inline"><mml:mrow><mml:mn mathvariant="normal">8.50</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M266" display="inline"><mml:mn mathvariant="normal">314</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M267" display="inline"><mml:mrow><mml:mn mathvariant="normal">2.18</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col3"><inline-formula><mml:math id="M268" display="inline"><mml:mn mathvariant="normal">254</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M269" display="inline"><mml:mrow><mml:mn mathvariant="normal">4.69</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5"><inline-formula><mml:math id="M270" display="inline"><mml:mn mathvariant="normal">232</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col6"><inline-formula><mml:math id="M271" display="inline"><mml:mrow><mml:mn mathvariant="normal">7.31</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
       </oasis:row>
       <oasis:row>
         <oasis:entry colname="col1"><inline-formula><mml:math id="M272" display="inline"><mml:mn mathvariant="normal">393</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col2"><inline-formula><mml:math id="M273" display="inline"><mml:mrow><mml:mn mathvariant="normal">1.93</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col3"><inline-formula><mml:math id="M274" display="inline"><mml:mn mathvariant="normal">318</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col4"><inline-formula><mml:math id="M275" display="inline"><mml:mrow><mml:mn mathvariant="normal">4.51</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col5"><inline-formula><mml:math id="M276" display="inline"><mml:mn mathvariant="normal">290</mml:mn></mml:math></inline-formula></oasis:entry>
         <oasis:entry colname="col6"><inline-formula><mml:math id="M277" display="inline"><mml:mrow><mml:mn mathvariant="normal">7.32</mml:mn><mml:mo>×</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:math></inline-formula></oasis:entry>
       </oasis:row>
     </oasis:tbody>
   </oasis:tgroup></oasis:table></table-wrap>

      <p id="d1e5298">Regarding the experimental results, it can be noted that the influence of
the relative humidity via the thermophoresis and diffusiophoresis
contribution on the CE is of first order. For the larger AP radii studied,
the CE increases by a factor of 4 when the relative humidity passes from
93.5 % to 71.1 % – filling up the Greenfield gap as the models predict. A
slight decline of the contribution of these two phoretic effects is observed
when the AP radius decreases – with the previous factor of 4 reducing to a
factor of 3 for the smaller AP radii and for the same relative humidity
range (from 93.5 % to 71.1 %). Although this decrease is small, it is in
line with the theory. Indeed, when the AP radius decreases the contribution
of the Brownian motion on the CE increases and starts dominating over the
thermophoretic and the diffusiophoretic forces. Consequently, the influence
of the relative humidity on the CE is negligible for nanometric AP radii.</p>
      <p id="d1e5302">Moreover, the impact of the AP size is lower than the influence of the
relative humidity for the experimental conditions considered. Indeed,
between the larger and the smaller AP radii, the CE is only increased by a
factor of 1.61, 1.59 and 2.03 for the respective relative humidity levels of
71.1 %, 82.4 % and 93.5 %. A decrease in the AP size effect on the CE is
noticeable when the thermophoresis and the diffusiophoresis contributions
intensify – in other words when the relative humidity declines. This
observation is in line with the modelling of the CE when a threshold is more
and more visible as the relative humidity decreases for the submicron AP
radii studied.</p>
      <p id="d1e5305">Finally, for the AP sizes and the droplet radius studied, both models
describe relatively well the observed CE variations when changing relative
humidity. For the two lowest levels of relative humidity (71.1 % and
82.4 %), the CE modelling is really close between both models since the
thermophoresis and diffusiophoresis dominate the influence on the CE.
Nevertheless, some significant discrepancies appear for the highest relative
humidity (93.5 %), where the Dépée et al. (2019) extended model
gives higher CE values. These differences result from the Wang et al. (1978)
model, which does not consider dynamic effects such as AP inertia, AP weight
and interception, in contrast to the extended model of Dépée et al. (2019), which offers a complete description of the microphysical effects
involved in clouds.</p>

      <?xmltex \floatpos{t}?><fig id="Ch1.F10"><?xmltex \currentcnt{10}?><?xmltex \def\figurename{Figure}?><label>Figure 10</label><caption><p id="d1e5310">CE measurements for three levels of relative humidity – 71.1 %, 82.4 %
and 93.5 % – compared to the extended model of Dépée et al. (2019) (solid lines) and the Wang et al. (1978) model (dashed line). Squares are the CE measurements summarised in Table 3. For the modelling, air
temperature and droplet radius are then the mean values of the three levels
of relative humidity – <inline-formula><mml:math id="M278" display="inline"><mml:mrow><mml:msub><mml:mi>T</mml:mi><mml:mtext>air</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:mn mathvariant="normal">0.26</mml:mn></mml:mrow></mml:math></inline-formula>, 0.27 and 1.2 <inline-formula><mml:math id="M279" display="inline"><mml:msup><mml:mi/><mml:mo>∘</mml:mo></mml:msup></mml:math></inline-formula>C – <inline-formula><mml:math id="M280" display="inline"><mml:mrow><mml:mi>A</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">49.3</mml:mn></mml:mrow></mml:math></inline-formula>, 50.8 and 48.8 <inline-formula><mml:math id="M281" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m – from the lowest to the highest,
respectively. For RH <inline-formula><mml:math id="M282" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 100 %, the parameters are those from Table 2.</p></caption>
          <?xmltex \igopts{width=184.942913pt}?><graphic xlink:href="https://acp.copernicus.org/articles/21/6945/2021/acp-21-6945-2021-f10.png"/>

        </fig>

</sec>
</sec>
<?pagebreak page6957?><sec id="Ch1.S5" sec-type="conclusions">
  <label>5</label><title>Conclusions</title>
      <p id="d1e5380">In-CASE (In-Cloud Aerosol Scavenging Experiment) was built to conduct a set
of experiments quantifying the contribution of any microphysics effects
involved in the AP collection by falling cloud droplets. For this purpose,
all parameters influencing the collection efficiency (CE) are controlled – i.e. the AP and droplet sizes, the AP and droplet electric charges, and the
relative humidity.</p>
      <p id="d1e5383">This study focused on the influence of relative humidity since the
literature lacks baseline data validating the theoretical models of CE
implemented in cloud, climate and pollution models. Indeed, only the work of
Ardon-Dryer et al. (2015) is dedicated to investigate the CE variation for
two levels of relative humidity and cloud droplet sizes (<inline-formula><mml:math id="M283" display="inline"><mml:mrow><mml:mi>A</mml:mi><mml:mo>≤</mml:mo><mml:mn mathvariant="normal">100</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M284" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m). Nevertheless, for the droplet radius considered, the authors conclude
that the electrostatic forces could have played a key role on their CE
measurements, since the APs and droplets are charged, however slightly.</p>
      <p id="d1e5406">In the new measured CE dataset that is presented here, the APs and droplets
are neutralised. There is no significant remaining electrostatic effect
considering the maximum residual AP and droplet charges for the droplet
radius examined (<inline-formula><mml:math id="M285" display="inline"><mml:mrow><mml:mi>A</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">49.6</mml:mn><mml:mo>±</mml:mo><mml:mn mathvariant="normal">1.3</mml:mn></mml:mrow></mml:math></inline-formula> <inline-formula><mml:math id="M286" display="inline"><mml:mrow class="unit"><mml:mi mathvariant="normal">µ</mml:mi></mml:mrow></mml:math></inline-formula>m), which is twice as larger as the one
studied by Ardon-Dryer et al. (2015). Here, three levels of relative
humidity were investigated – 71.1 %, 82.4 % and 93.5 % – which are typical
in-cloud conditions.</p>
      <p id="d1e5433">From the measurements obtained, it is clear that the relative humidity – through the thermophoretic and diffusiophoretic forces – significantly
impacts the CE. Indeed, an increase by a factor of 4 was observed for the CE
when the relative humidity level declines from 93.5 % to 71.1 %. Thus, it
is quite important to consider these effects in the cloud model since the levels
of relative humidity are comparable to those used in this study. It was
also shown that for the AP size considered in the present study, the impact
of the AP size on the CE is a second-order dependency. In fact, only a
doubling of the CE was highlighted – for a relative humidity of 93.5 % – from the larger to the smaller AP radius considered. This impact of the AP
size decreased when the influence of the relative humidity increases.</p>
      <p id="d1e5437">The CEs computed with the well-established model of Wang et al. (1978) as
well as the new Lagrangian model described in Dépée et al. (2019)
and extended to phoretic effects were compared to the measurements. The
agreement was good. Nevertheless, significant discrepancies between both
models were revealed for high relative humidity (in subsaturated air) where
the relative humidity influence is weak. This can be attributed to the fact
that the model of Wang et al. (1978) disregards some microphysics effects
such as AP weight, AP inertia and interception which have a significant
contribution near the Greenfield gap (Greenfield, 1957). Thus, the extended
Lagrangian model of Dépée et al. (2019) offers a more appropriate
estimation of the CE.</p>
      <p id="d1e5440">In this study, the electrostatic effects were not considered. However,
Dépée et al. (2019) have shown an impact of several orders of
magnitude on the CE, especially considering the electric charges of cloud
droplets and radioactive APs. Then, it is essential to investigate the AP
collection by clouds<?pagebreak page6958?> due to the electrostatic forces – referred to as
“electroscavenging”. Up to now, the analytical expression of the
electrostatic forces – based on the image charge theory developed by Jackson
(1999) – has never been experimentally validated or at least emphasised.
Consequently, In-CASE was also used to study the influence of the droplet
and AP charge on CE which is addressed in a second paper (Dépée et al., 2021).</p><?xmltex \hack{\clearpage}?>
</sec>

      
      </body>
    <back><app-group>

<?pagebreak page6959?><app id="App1.Ch1.S1">
  <?xmltex \currentcnt{A}?><label>Appendix A</label><title>Evaluation method of the collection efficiency in the presence
of multiple charged APs</title>
      <p id="d1e5455">This Appendix presents the method used to evaluate the CE when the selected
AP radius by the DMA is 50 or 150 nm – when the multiple charged APs cannot
be neglected (see Sect. 3.2).</p>
<sec id="App1.Ch1.S1.SS1">
  <label>A1</label><title>Ratio of multiple charged APs</title>
<sec id="App1.Ch1.S1.SS1.SSS1">
  <label>A1.1</label><?xmltex \opttitle{Selected AP radius of 50\,nm}?><title>Selected AP radius of 50 nm</title>
      <p id="d1e5473">Before the AP selection, the DMA charges the APs following a known charging
law (Wiedensohler, 1988) with an energy X-ray neutraliser (not presented in
Fig. 2).</p>
      <p id="d1e5476">The first step is to estimate the number and mass ratios of multiple charged
APs in the mean AP mass concentration measured in the In-CASE collision
chamber (<inline-formula><mml:math id="M287" display="inline"><mml:mrow><mml:msub><mml:mi>C</mml:mi><mml:mtext>m,AP</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>). For this purpose, the size distribution of the APs
produced by the atomiser is measured just before the DMA selection (Fig. 7). The AP number concentrations at the single (50 nm), double (75.8 nm),
triple (98.2 nm), quadruple (119.1 nm) and quintuple (139.1 nm) charged
radii are deduced from the size distribution.</p>
      <p id="d1e5490">Those AP number concentrations are the total concentrations at a given
multiple charged AP radius. From those total concentrations, a fraction will
be actually carrying the correct charge number to have the exact electrical
mobility selected by the DMA (one charge for 50 nm, two charges for 75.8 nm and three
charges for 98.2 nm, etc.). This fraction number (<inline-formula><mml:math id="M288" display="inline"><mml:mrow><mml:msub><mml:mi>F</mml:mi><mml:mrow><mml:mi>N</mml:mi><mml:mo>,</mml:mo><mml:mi>n</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>) of an AP radius
(<inline-formula><mml:math id="M289" display="inline"><mml:mi>a</mml:mi></mml:math></inline-formula>) carrying <inline-formula><mml:math id="M290" display="inline"><mml:mi>n</mml:mi></mml:math></inline-formula> elementary charge(s) can be estimated through the AP
charging law imposed by the energy X-ray neutraliser – defined by
Wiedensohler (1988). This similar Boltzmann distribution is defined in
Eq. (A1):
<?xmltex \hack{\allowdisplaybreaks}?>
              <disp-formula id="App1.Ch1.S1.E13" content-type="numbered"><label>A1</label><mml:math id="M291" display="block"><mml:mrow><mml:mfenced close="" open="{"><mml:mtable class="array" columnalign="center center"><mml:mtr><mml:mtd><mml:mrow><mml:msub><mml:mi>F</mml:mi><mml:mrow><mml:mi>N</mml:mi><mml:mo>,</mml:mo><mml:mi>n</mml:mi></mml:mrow></mml:msub><mml:mfenced close=")" open="("><mml:mi>a</mml:mi></mml:mfenced><mml:mo>=</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mfenced close="]" open="["><mml:mrow><mml:msubsup><mml:mo movablelimits="false">∑</mml:mo><mml:mrow><mml:mi>i</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow><mml:mn mathvariant="normal">6</mml:mn></mml:msubsup><mml:msub><mml:mi>c</mml:mi><mml:mi>i</mml:mi></mml:msub><mml:mfenced close=")" open="("><mml:mi>n</mml:mi></mml:mfenced><mml:msup><mml:mfenced close=")" open="("><mml:mrow><mml:mi>log⁡</mml:mi><mml:mfenced open="(" close=")"><mml:mstyle scriptlevel="+1"><mml:mfrac><mml:mrow><mml:mn mathvariant="normal">2</mml:mn><mml:mi>a</mml:mi></mml:mrow><mml:mrow><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">9</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:mfrac></mml:mstyle></mml:mfenced></mml:mrow></mml:mfenced><mml:mrow><mml:mi>i</mml:mi><mml:mo>-</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow></mml:msup></mml:mrow></mml:mfenced></mml:mrow></mml:msup></mml:mrow></mml:mtd><mml:mtd><mml:mtable class="array" columnalign="center center"><mml:mtr><mml:mtd><mml:mrow><mml:mtext>if</mml:mtext><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi>n</mml:mi><mml:mo>&lt;</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:mtd><mml:mtd><mml:mrow><mml:mfenced close="" open="{"><mml:mtable class="array" columnalign="center"><mml:mtr><mml:mtd><mml:mrow><mml:mspace linebreak="nobreak" width="0.125em"/><mml:msub><mml:mi>c</mml:mi><mml:mrow><mml:mi>i</mml:mi><mml:mo>∈</mml:mo><mml:mo>[</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">6</mml:mn><mml:mo>]</mml:mo></mml:mrow></mml:msub><mml:mfenced close=")" open="("><mml:mn mathvariant="normal">1</mml:mn></mml:mfenced><mml:mo>=</mml:mo><mml:mfenced close="]" open="["><mml:mtable class="array" columnalign="center"><mml:mtr><mml:mtd><mml:mtable class="array" columnalign="center"><mml:mtr><mml:mtd><mml:mtable class="array" columnalign="center"><mml:mtr><mml:mtd><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">2</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">3484</mml:mn></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:mn mathvariant="normal">0</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">6044</mml:mn></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:mn mathvariant="normal">0</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">4800</mml:mn></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:mn mathvariant="normal">0</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">0013</mml:mn></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mtable class="array" columnalign="center"><mml:mtr><mml:mtd><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">0</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">1553</mml:mn></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:mn mathvariant="normal">0</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">0320</mml:mn></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:mtd></mml:mtr></mml:mtable></mml:mfenced></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:msub><mml:mi>c</mml:mi><mml:mrow><mml:mi>i</mml:mi><mml:mo>∈</mml:mo><mml:mo>[</mml:mo><mml:mn mathvariant="normal">1</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">6</mml:mn><mml:mo>]</mml:mo></mml:mrow></mml:msub><mml:mfenced open="(" close=")"><mml:mn mathvariant="normal">2</mml:mn></mml:mfenced><mml:mo>=</mml:mo><mml:mfenced open="[" close="]"><mml:mtable class="array" columnalign="center"><mml:mtr><mml:mtd><mml:mtable class="array" columnalign="center"><mml:mtr><mml:mtd><mml:mtable class="array" columnalign="center"><mml:mtr><mml:mtd><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">44</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">4756</mml:mn></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:mn mathvariant="normal">79</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">3772</mml:mn></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">62</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">8900</mml:mn></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:mn mathvariant="normal">26</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">4492</mml:mn></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mtable class="array" columnalign="center"><mml:mtr><mml:mtd><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">5</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">7480</mml:mn></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:mn mathvariant="normal">0</mml:mn><mml:mo>,</mml:mo><mml:mn mathvariant="normal">5049</mml:mn></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:mtd></mml:mtr></mml:mtable></mml:mfenced></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:mfenced></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:msub><mml:mi>F</mml:mi><mml:mrow><mml:mi>N</mml:mi><mml:mo>,</mml:mo><mml:mi>n</mml:mi></mml:mrow></mml:msub><mml:mfenced open="(" close=")"><mml:mi>a</mml:mi></mml:mfenced><mml:mo>=</mml:mo><mml:mstyle displaystyle="false"><mml:mstyle displaystyle="false"><mml:mfrac style="text"><mml:mi>e</mml:mi><mml:msqrt><mml:mrow><mml:mn mathvariant="normal">8</mml:mn><mml:msup><mml:mi mathvariant="italic">π</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:msub><mml:mi mathvariant="italic">ε</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mi>a</mml:mi><mml:msub><mml:mi>k</mml:mi><mml:mtext>b</mml:mtext></mml:msub><mml:msub><mml:mi>T</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow></mml:msqrt></mml:mfrac></mml:mstyle></mml:mstyle><mml:msup><mml:mi>exp⁡</mml:mi><mml:mrow><mml:mo>-</mml:mo><mml:mstyle scriptlevel="+1"><mml:mfrac><mml:mrow><mml:msup><mml:mfenced open="[" close="]"><mml:mrow><mml:mi>n</mml:mi><mml:mo>-</mml:mo><mml:mfrac><mml:mrow><mml:mn mathvariant="normal">4</mml:mn><mml:mi mathvariant="italic">π</mml:mi><mml:msub><mml:mi mathvariant="italic">ε</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mi>a</mml:mi><mml:msub><mml:mi>k</mml:mi><mml:mtext>b</mml:mtext></mml:msub><mml:msub><mml:mi>T</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow><mml:mrow><mml:msup><mml:mi>e</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:mrow></mml:mfrac><mml:mi>l</mml:mi><mml:mi>n</mml:mi><mml:mfenced close=")" open="("><mml:mfrac><mml:mrow><mml:msub><mml:mi>Z</mml:mi><mml:mrow><mml:mi>i</mml:mi><mml:mo>+</mml:mo></mml:mrow></mml:msub></mml:mrow><mml:mrow><mml:msub><mml:mi>Z</mml:mi><mml:mrow><mml:mi>i</mml:mi><mml:mo>-</mml:mo></mml:mrow></mml:msub></mml:mrow></mml:mfrac></mml:mfenced></mml:mrow></mml:mfenced><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:mrow><mml:mrow><mml:mn mathvariant="normal">2</mml:mn><mml:mfrac><mml:mrow><mml:mn mathvariant="normal">4</mml:mn><mml:mi mathvariant="italic">π</mml:mi><mml:msub><mml:mi mathvariant="italic">ε</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub><mml:mi>a</mml:mi><mml:msub><mml:mi>k</mml:mi><mml:mtext>b</mml:mtext></mml:msub><mml:msub><mml:mi>T</mml:mi><mml:mtext>air</mml:mtext></mml:msub></mml:mrow><mml:mrow><mml:msup><mml:mi>e</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msup></mml:mrow></mml:mfrac></mml:mrow></mml:mfrac></mml:mstyle></mml:mrow></mml:msup></mml:mrow></mml:mtd><mml:mtd><mml:mrow><mml:mtext>if</mml:mtext><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi>n</mml:mi><mml:mo>≥</mml:mo><mml:mn mathvariant="normal">3</mml:mn><mml:mo>,</mml:mo></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:mfenced></mml:mrow></mml:math></disp-formula>
            <?xmltex \hack{\newpage}?><?xmltex \hack{\noindent}?>where <inline-formula><mml:math id="M292" display="inline"><mml:mrow><mml:msub><mml:mi mathvariant="italic">ε</mml:mi><mml:mn mathvariant="normal">0</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>, <inline-formula><mml:math id="M293" display="inline"><mml:mrow><mml:msub><mml:mi>k</mml:mi><mml:mtext>b</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> and <inline-formula><mml:math id="M294" display="inline"><mml:mrow><mml:msub><mml:mi>T</mml:mi><mml:mtext>air</mml:mtext></mml:msub><mml:mo>≈</mml:mo><mml:mn mathvariant="normal">295.15</mml:mn></mml:mrow></mml:math></inline-formula> K are the vacuum permittivity, the Boltzmann constant and the lab temperature. The
ion mobility ratio (<inline-formula><mml:math id="M295" display="inline"><mml:mstyle displaystyle="false"><mml:mfrac style="text"><mml:mrow><mml:msub><mml:mi>Z</mml:mi><mml:mrow><mml:mi>i</mml:mi><mml:mo>+</mml:mo></mml:mrow></mml:msub></mml:mrow><mml:mrow><mml:msub><mml:mi>Z</mml:mi><mml:mrow><mml:mi>i</mml:mi><mml:mo>-</mml:mo></mml:mrow></mml:msub></mml:mrow></mml:mfrac></mml:mstyle></mml:math></inline-formula>) is assumed to be equal to 0.875
(Wiedensohler, 1988).</p>
      <p id="d1e6049">Finally, the effective AP numbers for the respective multiple charged AP
radii have been evaluated in the AP flow at the DMA's outlet (corresponding
to the AP flow going into the In-CASE collision chamber). Thus, the mass
fractions (<inline-formula><mml:math id="M296" display="inline"><mml:mrow><mml:msub><mml:mi>F</mml:mi><mml:mtext>m,n</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) for the single, double, triple, quadruple and quintuple
charged AP radii were estimated. It was found that the quadruple and
quintuple charged AP radii can be neglected since their weight is less than 6 % in the mean AP mass concentration in the In-CASE collision chamber
(<inline-formula><mml:math id="M297" display="inline"><mml:mrow><mml:msub><mml:mi>C</mml:mi><mml:mtext>m,AP</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>). Moreover, since their number concentrations are
really poor (less than 50 cm<inline-formula><mml:math id="M298" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>) compared to the single, double and
triple charged radius (<inline-formula><mml:math id="M299" display="inline"><mml:mrow><mml:mo>∼</mml:mo><mml:msup><mml:mn mathvariant="normal">10</mml:mn><mml:mn mathvariant="normal">3</mml:mn></mml:msup></mml:mrow></mml:math></inline-formula>–10<inline-formula><mml:math id="M300" display="inline"><mml:msup><mml:mi/><mml:mn mathvariant="normal">4</mml:mn></mml:msup></mml:math></inline-formula> cm<inline-formula><mml:math id="M301" display="inline"><mml:msup><mml:mi/><mml:mrow><mml:mo>-</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:msup></mml:math></inline-formula>), the likelihood
of those APs being collected by a droplet in the collision chamber is
extremely small.</p>
</sec>
</sec>
<sec id="App1.Ch1.S1.SS2">
  <label>A2</label><?xmltex \opttitle{Selected AP radius of 150\,nm}?><title>Selected AP radius of 150 nm</title>
      <p id="d1e6131">For a selected AP radius of 150 nm, only the double charged APs are
considered since the triple charged APs are assumed to be stopped by the
impactor at the DMA's inlet (triple charged radius <inline-formula><mml:math id="M302" display="inline"><mml:mo>=</mml:mo></mml:math></inline-formula> 353.4 nm and <inline-formula><mml:math id="M303" display="inline"><mml:mrow><mml:msub><mml:mi>D</mml:mi><mml:mrow><mml:mn mathvariant="normal">50</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi mathvariant="italic">%</mml:mi></mml:mrow></mml:msub><mml:mo>/</mml:mo><mml:mn mathvariant="normal">2</mml:mn><mml:mo>=</mml:mo><mml:mn mathvariant="normal">213</mml:mn></mml:mrow></mml:math></inline-formula> nm, Table 1). The mass fractions (<inline-formula><mml:math id="M304" display="inline"><mml:mrow><mml:msub><mml:mi>F</mml:mi><mml:mtext>m,n</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) of the single and
double charged APs are evaluated in the same way as a 50 nm selected AP radius.</p><?xmltex \hack{\newpage}?>
</sec>
<?pagebreak page6960?><sec id="App1.Ch1.S1.SS3">
  <label>A3</label><title>Deduction of the collection efficiency</title>
</sec>
<sec id="App1.Ch1.S1.SS4">
  <label>A4</label><?xmltex \opttitle{Selected AP radius of 50\,nm}?><title>Selected AP radius of 50 nm</title>
      <p id="d1e6194">As explained in Sect. 3.2, when the selected AP radius by the DMA is
50 nm, the AP mass collected at the In-CASE chamber bottom (<inline-formula><mml:math id="M305" display="inline"><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,d</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) is
actually the sum of the masses of the single (50 nm), double (75.8 nm) and
triple (98.2 nm) charged AP collected by the droplet train. This can also be
defined as the linear combination of the collection efficiencies
(CE<inline-formula><mml:math id="M306" display="inline"><mml:mrow><mml:msub><mml:mi/><mml:mi>i</mml:mi></mml:msub><mml:mfenced open="(" close=")"><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mi>i</mml:mi></mml:msub><mml:mo>,</mml:mo><mml:mi>A</mml:mi><mml:mo>,</mml:mo><mml:mtext>RH</mml:mtext></mml:mrow></mml:mfenced></mml:mrow></mml:math></inline-formula>) and the available AP mass in the
volume swept by the droplets (<inline-formula><mml:math id="M307" display="inline"><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,available</mml:mtext></mml:msub><mml:mfenced open="(" close=")"><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:mfenced></mml:mrow></mml:math></inline-formula>) at a
given multiple charged dry AP radius (<inline-formula><mml:math id="M308" display="inline"><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:math></inline-formula>) – Eq. (A2):
            <disp-formula id="App1.Ch1.S1.E14" content-type="numbered"><label>A2</label><mml:math id="M309" display="block"><mml:mtable columnspacing="1em" class="split" rowspacing="0.2ex" displaystyle="true" columnalign="right left"><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,d</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:msub><mml:mi>m</mml:mi><mml:mtext>50 nm,d</mml:mtext></mml:msub><mml:mo>+</mml:mo><mml:msub><mml:mi>m</mml:mi><mml:mtext>75.8 nm,d</mml:mtext></mml:msub><mml:mo>+</mml:mo><mml:msub><mml:mi>m</mml:mi><mml:mtext>98.2 nm,d</mml:mtext></mml:msub></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:mo>=</mml:mo><mml:munderover><mml:mo movablelimits="false">∑</mml:mo><mml:mrow><mml:mi>i</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow><mml:mn mathvariant="normal">3</mml:mn></mml:munderover><mml:msub><mml:mtext>CE</mml:mtext><mml:mi>i</mml:mi></mml:msub><mml:mfenced open="(" close=")"><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mi>i</mml:mi></mml:msub><mml:mo>,</mml:mo><mml:mi>A</mml:mi><mml:mo>,</mml:mo><mml:mtext>RH</mml:mtext></mml:mrow></mml:mfenced><mml:mo>×</mml:mo><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,available</mml:mtext></mml:msub><mml:mfenced close=")" open="("><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:mfenced><mml:mo>,</mml:mo></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula>
          where the respective available AP masses in the volume swept by the droplets
are defined by Eq. (A3):
            <disp-formula id="App1.Ch1.S1.E15" content-type="numbered"><label>A3</label><mml:math id="M310" display="block"><mml:mtable rowspacing="0.2ex" class="split" columnspacing="1em" displaystyle="true" columnalign="right left"><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,available</mml:mtext></mml:msub><mml:mfenced open="(" close=")"><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:mfenced><mml:mo>=</mml:mo><mml:mi mathvariant="italic">π</mml:mi><mml:msup><mml:mfenced close=")" open="("><mml:mrow><mml:mi>A</mml:mi><mml:mo>+</mml:mo><mml:mtext>GroF(RH)</mml:mtext><mml:mo>×</mml:mo><mml:msub><mml:mi>a</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:mfenced><mml:mn mathvariant="normal">2</mml:mn></mml:msup><mml:mo>×</mml:mo><mml:msub><mml:mi>F</mml:mi><mml:mi>d</mml:mi></mml:msub></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:mo>×</mml:mo><mml:mi mathvariant="normal">Δ</mml:mi><mml:mi>t</mml:mi><mml:mo>×</mml:mo><mml:msub><mml:mi>H</mml:mi><mml:mtext>eff</mml:mtext></mml:msub><mml:mo>×</mml:mo><mml:msub><mml:mi>C</mml:mi><mml:mtext>m,AP</mml:mtext></mml:msub><mml:mo>×</mml:mo><mml:msub><mml:mi>F</mml:mi><mml:mrow><mml:mi>m</mml:mi><mml:mo>,</mml:mo><mml:mi>n</mml:mi></mml:mrow></mml:msub><mml:mfenced open="(" close=")"><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:mfenced><mml:mo>.</mml:mo></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula></p>
      <p id="d1e6448">All the parameters given in Eqs. (A2) and (A3) are either measured or
initially known, except the collection efficiencies (CE<inline-formula><mml:math id="M311" display="inline"><mml:msub><mml:mi/><mml:mi>i</mml:mi></mml:msub></mml:math></inline-formula>) for the
single, double and triple charged AP dry radius. To deduce those three
unknown parameters, a set of <inline-formula><mml:math id="M312" display="inline"><mml:mi>j</mml:mi></mml:math></inline-formula> linearly independent experiments (<inline-formula><mml:math id="M313" display="inline"><mml:mrow><mml:mi>j</mml:mi><mml:mo>≥</mml:mo><mml:mn mathvariant="normal">3</mml:mn></mml:mrow></mml:math></inline-formula>) has been performed by varying the ratio of the multiple charged APs (by
changing the AP size distribution mode in Fig. 7). The matrix system is
then described through Eq. (A4):
            <disp-formula id="App1.Ch1.S1.E16" content-type="numbered"><label>A4</label><mml:math id="M314" display="block"><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mtext>collected mass</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:msub><mml:mi>M</mml:mi><mml:mtext>available</mml:mtext></mml:msub><mml:mo>×</mml:mo><mml:msub><mml:mi>M</mml:mi><mml:mtext>CE</mml:mtext></mml:msub><mml:mo>,</mml:mo></mml:mrow></mml:math></disp-formula>
          where the one-dimension matrix of the collected mass (<inline-formula><mml:math id="M315" display="inline"><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mtext>collected 
mass</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) for the set of <inline-formula><mml:math id="M316" display="inline"><mml:mi>j</mml:mi></mml:math></inline-formula> experiment is noted as Eq. (A5):
            <disp-formula id="App1.Ch1.S1.E17" content-type="numbered"><label>A5</label><mml:math id="M317" display="block"><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mtext>collected  mass</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:mfenced close="]" open="["><mml:mtable class="array" columnalign="center"><mml:mtr><mml:mtd><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,d,1</mml:mtext></mml:msub></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mi mathvariant="normal">⋮</mml:mi></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mrow><mml:mtext>AP,d,</mml:mtext><mml:mi>j</mml:mi></mml:mrow></mml:msub></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:mfenced><mml:mo>.</mml:mo></mml:mrow></mml:math></disp-formula></p>
      <p id="d1e6564">The two-dimension matrix of the available AP masses in the volume swept by
the droplet (<inline-formula><mml:math id="M318" display="inline"><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mtext>available</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) for the single (<inline-formula><mml:math id="M319" display="inline"><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>), double (<inline-formula><mml:math id="M320" display="inline"><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>) and
triple (<inline-formula><mml:math id="M321" display="inline"><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:math></inline-formula>) charged is defined as Eq. (A6):
            <disp-formula id="App1.Ch1.S1.E18" content-type="numbered"><label>A6</label><mml:math id="M322" display="block"><mml:mtable columnspacing="1em" rowspacing="0.2ex" class="split" displaystyle="true" columnalign="right left"><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mtext>available</mml:mtext></mml:msub></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><?xmltex \hack{\hbox\bgroup\fontsize{7.7}{7.7}\selectfont$\displaystyle}?><mml:mo>=</mml:mo><mml:mfenced open="[" close="]"><mml:mtable class="array" columnalign="center center center"><mml:mtr><mml:mtd><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,available,1</mml:mtext></mml:msub><mml:mfenced close=")" open="("><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub></mml:mrow></mml:mfenced></mml:mrow></mml:mtd><mml:mtd><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,available,1</mml:mtext></mml:msub><mml:mfenced close=")" open="("><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:mfenced></mml:mrow></mml:mtd><mml:mtd><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,available,1</mml:mtext></mml:msub><mml:mfenced open="(" close=")"><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:mfenced></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mi mathvariant="normal">⋮</mml:mi></mml:mtd><mml:mtd><mml:mi mathvariant="normal">⋮</mml:mi></mml:mtd><mml:mtd><mml:mi mathvariant="normal">⋮</mml:mi></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mrow><mml:mtext>AP,available</mml:mtext><mml:mo>,</mml:mo><mml:mi>j</mml:mi></mml:mrow></mml:msub><mml:mfenced close=")" open="("><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mn mathvariant="normal">1</mml:mn></mml:msub></mml:mrow></mml:mfenced></mml:mrow></mml:mtd><mml:mtd><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mrow><mml:mtext>AP,available</mml:mtext><mml:mo>,</mml:mo><mml:mi>j</mml:mi></mml:mrow></mml:msub><mml:mfenced close=")" open="("><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:mfenced></mml:mrow></mml:mtd><mml:mtd><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mrow><mml:mtext>AP,available</mml:mtext><mml:mo>,</mml:mo><mml:mi>j</mml:mi></mml:mrow></mml:msub><mml:mfenced close=")" open="("><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:mfenced></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:mfenced><mml:mo>.</mml:mo><?xmltex \hack{$\egroup}?></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula></p>
      <p id="d1e6749">The one-dimension matrix containing all the unknown CEs (<inline-formula><mml:math id="M323" display="inline"><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mtext>CE</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) is
Eq. (A7):
            <disp-formula id="App1.Ch1.S1.E19" content-type="numbered"><label>A7</label><mml:math id="M324" display="block"><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mtext>CE</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:mfenced close="]" open="["><mml:mtable class="array" columnalign="center"><mml:mtr><mml:mtd><mml:mrow><mml:msub><mml:mtext>CE</mml:mtext><mml:mn mathvariant="normal">1</mml:mn></mml:msub></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:msub><mml:mtext>CE</mml:mtext><mml:mn mathvariant="normal">2</mml:mn></mml:msub></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd><mml:mrow><mml:msub><mml:mtext>CE</mml:mtext><mml:mn mathvariant="normal">3</mml:mn></mml:msub></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:mfenced><mml:mo>.</mml:mo></mml:mrow></mml:math></disp-formula></p>
      <p id="d1e6803">Finally, this matrix system (16) is numerically solved by the quasi-Newton
method. The uniqueness of the solution was verified – the initial value was
changed in the solving method, giving the same solution vector.</p>
<sec id="App1.Ch1.S1.SS4.SSS1">
  <label>A4.1</label><?xmltex \opttitle{Selected AP radius of 150\,nm}?><title>Selected AP radius of 150 nm</title>
      <p id="d1e6814">Like the same principle as before, the AP mass collected by the whole
droplets (<inline-formula><mml:math id="M325" display="inline"><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,d</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula>) is the linear combination of the single (150 nm) and
double charged (253.7 nm), defined as Eq. (A8):
              <disp-formula id="App1.Ch1.S1.E20" content-type="numbered"><label>A8</label><mml:math id="M326" display="block"><mml:mtable class="split" rowspacing="0.2ex" columnspacing="1em" displaystyle="true" columnalign="right left"><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,d</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:msub><mml:mi>m</mml:mi><mml:mtext>150 nm,d</mml:mtext></mml:msub><mml:mo>+</mml:mo><mml:msub><mml:mi>m</mml:mi><mml:mtext>253.7 nm,d</mml:mtext></mml:msub><mml:mo>=</mml:mo><mml:munderover><mml:mo movablelimits="false">∑</mml:mo><mml:mrow><mml:mi>i</mml:mi><mml:mo>=</mml:mo><mml:mn mathvariant="normal">1</mml:mn></mml:mrow><mml:mn mathvariant="normal">2</mml:mn></mml:munderover><mml:msub><mml:mtext>CE</mml:mtext><mml:mi>i</mml:mi></mml:msub><mml:mfenced close=")" open="("><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mi>i</mml:mi></mml:msub><mml:mo>,</mml:mo><mml:mtext>A,RH</mml:mtext></mml:mrow></mml:mfenced></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:mo>×</mml:mo><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,available</mml:mtext></mml:msub><mml:mfenced close=")" open="("><mml:mrow><mml:msub><mml:mi>a</mml:mi><mml:mi>i</mml:mi></mml:msub></mml:mrow></mml:mfenced><mml:mo>.</mml:mo></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula></p>
      <p id="d1e6906">Nevertheless, to avoid additional experiments and numerically reverse a
similar matrix system to (10), it was assumed that the CE of a dry AP radius
of 253.7 nm is equivalent to the one for a dry AP radius of 250 nm. Then,
the CE for a 150 nm dry AP radius is deduced by Eq. (A9):
              <disp-formula id="App1.Ch1.S1.E21" content-type="numbered"><label>A9</label><mml:math id="M327" display="block"><mml:mtable class="split" rowspacing="0.2ex" columnspacing="1em" displaystyle="true" columnalign="right left"><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><mml:msub><mml:mtext>CE</mml:mtext><mml:mn mathvariant="normal">1</mml:mn></mml:msub><mml:mfenced open="(" close=")"><mml:mrow><mml:mn mathvariant="normal">150</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi mathvariant="normal">nm</mml:mi><mml:mo>,</mml:mo><mml:mi>A</mml:mi><mml:mo>,</mml:mo><mml:mtext>RH</mml:mtext></mml:mrow></mml:mfenced></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><?xmltex \hack{\hbox\bgroup\fontsize{8.7}{8.7}\selectfont$\displaystyle}?><mml:mo>=</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,d</mml:mtext></mml:msub><mml:mo>-</mml:mo><mml:msub><mml:mtext>CE</mml:mtext><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mfenced open="(" close=")"><mml:mrow><mml:mn mathvariant="normal">253.7</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi mathvariant="normal">nm</mml:mi><mml:mo>,</mml:mo><mml:mi>A</mml:mi><mml:mo>,</mml:mo><mml:mtext>RH</mml:mtext></mml:mrow></mml:mfenced><mml:mo>×</mml:mo><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,available</mml:mtext></mml:msub><mml:mfenced close=")" open="("><mml:mrow><mml:mn mathvariant="normal">253.7</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow></mml:mfenced></mml:mrow><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,available</mml:mtext></mml:msub><mml:mfenced close=")" open="("><mml:mrow><mml:mn mathvariant="normal">150</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow></mml:mfenced></mml:mrow></mml:mfrac></mml:mstyle><?xmltex \hack{$\egroup}?></mml:mrow></mml:mtd></mml:mtr><mml:mtr><mml:mtd/><mml:mtd><mml:mrow><?xmltex \hack{\hbox\bgroup\fontsize{8.7}{8.7}\selectfont$\displaystyle}?><mml:mo>≈</mml:mo><mml:mstyle displaystyle="true"><mml:mfrac style="display"><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,d</mml:mtext></mml:msub><mml:mo>-</mml:mo><mml:mtext>CE</mml:mtext><mml:mfenced close=")" open="("><mml:mrow><mml:mn mathvariant="normal">250</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi mathvariant="normal">nm</mml:mi><mml:mo>,</mml:mo><mml:mi>A</mml:mi><mml:mo>,</mml:mo><mml:mtext>RH</mml:mtext></mml:mrow></mml:mfenced><mml:mo>×</mml:mo><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,available</mml:mtext></mml:msub><mml:mfenced open="(" close=")"><mml:mrow><mml:mn mathvariant="normal">253.7</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow></mml:mfenced></mml:mrow><mml:mrow><mml:msub><mml:mi>m</mml:mi><mml:mtext>AP,available</mml:mtext></mml:msub><mml:mfenced close=")" open="("><mml:mrow><mml:mn mathvariant="normal">150</mml:mn><mml:mspace width="0.125em" linebreak="nobreak"/><mml:mi mathvariant="normal">nm</mml:mi></mml:mrow></mml:mfenced></mml:mrow></mml:mfrac></mml:mstyle><?xmltex \hack{$\egroup}?><mml:mo>.</mml:mo></mml:mrow></mml:mtd></mml:mtr></mml:mtable></mml:math></disp-formula></p>
      <p id="d1e7067">The right term in Eq. (A9) has no unknown since the CE of a 250 nm dry AP
radius (CE<inline-formula><mml:math id="M328" display="inline"><mml:mrow><mml:msub><mml:mi/><mml:mn mathvariant="normal">2</mml:mn></mml:msub><mml:mfenced open="(" close=")"><mml:mtext>250  nm,A,RH </mml:mtext></mml:mfenced></mml:mrow></mml:math></inline-formula>) has been previously
calculated with the method developed in Sect. 3.1.</p><?xmltex \hack{\clearpage}?>
</sec>
</sec>
</app>

<?pagebreak page6961?><app id="App1.Ch1.S2">
  <?xmltex \currentcnt{B}?><label>Appendix B</label><title>Uncertainty of the collection efficiency in the presence of
multiple charged APs</title>
      <p id="d1e7094">This appendix presents the method used to evaluate the CE uncertainty when
the selected AP radius by the DMA is 50 or 150 nm – when the multiple
charged APs cannot be neglected (see Sect. 3.2).</p>
<sec id="App1.Ch1.S2.SS1">
  <label>B1</label><?xmltex \opttitle{With a selected dry AP radius of 150\,nm}?><title>With a selected dry AP radius of 150 nm</title>
      <p id="d1e7105">Since the CE of a selected dry AP radius of 150 nm (CE (150 nm, <inline-formula><mml:math id="M329" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>, RH)) is calculated through the CE of a selected dry AP radius of 250 nm (CE (250 nm, <inline-formula><mml:math id="M330" display="inline"><mml:mi>A</mml:mi></mml:math></inline-formula>, RH)) – Eq. (A9) – the uncertainty on the
CE for the 150 nm
(<inline-formula><mml:math id="M331" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mrow><mml:mtext>CE</mml:mtext><mml:mo>(</mml:mo><mml:mn mathvariant="normal">150</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi mathvariant="normal">nm</mml:mi><mml:mo>,</mml:mo><mml:mi>A</mml:mi><mml:mo>,</mml:mo><mml:mtext>RH</mml:mtext><mml:mo>)</mml:mo></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>)
is evaluated by
propagating the uncertainty on the CE for 250 nm (<inline-formula><mml:math id="M332" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mrow><mml:mtext>CE</mml:mtext><mml:mo>(</mml:mo><mml:mn mathvariant="normal">550</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi mathvariant="normal">nm</mml:mi><mml:mo>,</mml:mo><mml:mi>A</mml:mi><mml:mo>,</mml:mo><mml:mtext>RH</mml:mtext><mml:mo>)</mml:mo></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>). It means the term <inline-formula><mml:math id="M333" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mrow><mml:mtext>CE</mml:mtext><mml:mo>(</mml:mo><mml:mn mathvariant="normal">250</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi mathvariant="normal">nm</mml:mi><mml:mo>,</mml:mo><mml:mi>A</mml:mi><mml:mo>,</mml:mo><mml:mtext>HR</mml:mtext><mml:mo>)</mml:mo></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula> is added in
Eq. (8) to deduce
<inline-formula><mml:math id="M334" display="inline"><mml:mrow><mml:msub><mml:mi>u</mml:mi><mml:mrow><mml:mtext>CE</mml:mtext><mml:mo>(</mml:mo><mml:mn mathvariant="normal">150</mml:mn><mml:mspace linebreak="nobreak" width="0.125em"/><mml:mi mathvariant="normal">nm</mml:mi><mml:mo>,</mml:mo><mml:mi>A</mml:mi><mml:mo>,</mml:mo><mml:mtext>HR</mml:mtext><mml:mo>)</mml:mo></mml:mrow></mml:msub></mml:mrow></mml:math></inline-formula>.</p>
</sec>
<sec id="App1.Ch1.S2.SS2">
  <label>B2</label><?xmltex \opttitle{With a selected dry AP radius of 50\,nm}?><title>With a selected dry AP radius of 50 nm</title>
      <p id="d1e7248">When the selected dry AP radius is 50 nm, the matrix system (16), solved by
a quasi-Newton method, is composed of parameters each with their relative
uncertainties. The relative CE uncertainties of the single (50 nm), double
(75.8 nm) and triple (98.2 nm) charged dry AP radius are then deduced by
randomly perturbing the terms of the matrix <inline-formula><mml:math id="M335" display="inline"><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mtext>collected  mass</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> and
<inline-formula><mml:math id="M336" display="inline"><mml:mrow><mml:msub><mml:mi>M</mml:mi><mml:mtext>available</mml:mtext></mml:msub></mml:mrow></mml:math></inline-formula> in Eq. (A4) within the limits of their respective
experimental relative uncertainties. A total of 10 000 perturbed matrix systems were
generated by the Monte Carlo method and solved with the quasi-Newton method.
From the 10 000 solution vectors – shaped like Eq. (A5) – the ones
with negative CEs were removed since they have no physical meaning.
Figure B1 shows the set of the solutions for a relative humidity level of
71.1 % and a single charged dry AP radius (50 nm).</p>
      <p id="d1e7273">Finally, the relative uncertainty of the CE is given by the standard
deviation (<inline-formula><mml:math id="M337" display="inline"><mml:mi mathvariant="italic">σ</mml:mi></mml:math></inline-formula>) of the solution distribution.</p>

      <?xmltex \floatpos{t}?><fig id="App1.Ch1.S2.F11"><?xmltex \currentcnt{B1}?><?xmltex \def\figurename{Figure}?><label>Figure B1</label><caption><p id="d1e7285">Distribution of 10 000 solutions (negative values were removed)
for a relative humidity level of 71.1 % and a single charged dry AP
radius (50 nm).</p></caption>
          <?xmltex \igopts{width=236.157874pt}?><graphic xlink:href="https://acp.copernicus.org/articles/21/6945/2021/acp-21-6945-2021-f11.png"/>

        </fig>

<?xmltex \hack{\clearpage}?>
</sec>
</app>
  </app-group><notes notes-type="codeavailability"><title>Code availability</title>

      <p id="d1e7301">No code was developed in the present article. The code used was described in Dépée et al. (2019), published in the Journal of Aerosol Science, <uri>https://doi.org/10.1016/j.jaerosci.2019.04.001</uri>.</p>
  </notes><notes notes-type="dataavailability"><title>Data availability</title>

      <p id="d1e7310">All the underlying research data can be found in the present article.</p>
  </notes><notes notes-type="authorcontribution"><title>Author contributions</title>

      <p id="d1e7316">This work relies on the experimental work of AD, with a methodology and a conceptualization made in collaboration with PL. Formal analysis was also performed by AD and PL. Numerical simulations were performed by AD and TG. The original article was written by AD under the supervision of PL, MM and AF.</p>
  </notes><notes notes-type="competinginterests"><title>Competing interests</title>

      <p id="d1e7322">The authors declare that they have no conflict of interest.</p>
  </notes><ack><title>Acknowledgements</title><p id="d1e7328">Authors sincerely thank Luis A. Ladino for all the advice he provided for the design of In-CASE.</p></ack><notes notes-type="financialsupport"><title>Financial support</title>

      <p id="d1e7333">This work was funded by the French Institute for Radiological Protection and Nuclear Safety (IRSN).</p>
  </notes><notes notes-type="reviewstatement"><title>Review statement</title>

      <p id="d1e7339">This paper was edited by Joachim Curtius and reviewed by two anonymous referees.</p>
  </notes><ref-list>
    <title>References</title>

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  </ref-list></back>
    <!--<article-title-html>Laboratory study of the collection efficiency of submicron aerosol particles by cloud droplets – Part I: Influence of relative humidity</article-title-html>
<abstract-html><p>A new In-Cloud Aerosol Scavenging Experiment (In-CASE) has been conceived to
measure the collection efficiency (CE) of submicron aerosol particles by
cloud droplets. In this setup, droplets fall at their terminal velocity
through a 1&thinsp;m high chamber in a laminar flow containing aerosol
particles. At the bottom of the In-CASE chamber, the droplet train is
separated from the aerosol particle flow – droplets are collected in an
impaction cup, whereas aerosol particles are deposited on a high-efficiency
particulate air (HEPA) filter. The collected droplets and the filter are
then analysed by fluorescence spectrometry since the aerosol particles are
atomised from a sodium fluorescein salt solution
(C<sub>20</sub>H<sub>10</sub>Na<sub>2</sub>O<sub>5</sub>). In-CASE fully controls all the parameters
which affect the CE – the droplets and aerosol particles size distributions
are monodispersed, the electric charges of droplets and aerosol particles
are controlled, and the relative humidity is indirectly set via the
chamber's temperature. This novel In-CASE setup is presented here as well as
the first measurements obtained to study the impact of relative humidity on
CE. For this purpose, droplets and particles are electrically neutralised. A
droplet radius of 49.6±1.3&thinsp;µm has been considered for six
particle dry radii between 50 and 250&thinsp;nm and three relative humidity levels
of 71.1±1.3&thinsp;%, 82.4±1.4&thinsp;% and 93.5±0.9&thinsp;%. These new
CE measurements have been compared to theoretical models from literature
which adequately describe the relative humidity influence on the measured
CE.</p></abstract-html>
<ref-html id="bib1.bib1"><label>1</label><mixed-citation>
Adachi, K., Kajino, M., Zaizen, Y., and Igarashi, Y.: Emission of spherical
cesium-bearing particles from an early stage of the Fukushima nuclear
accident, Sci. Rep.-UK, 3, 1–5, <a href="https://doi.org/doi.org/10.1038/srep02554" target="_blank">https://doi.org/doi.org/10.1038/srep02554</a>, 2013.
</mixed-citation></ref-html>
<ref-html id="bib1.bib2"><label>2</label><mixed-citation>
Al-Azzawi, H. K. and Owen, I.: Measuring the thermal conducitivity of
uranin, Int. J. Heat Fluid Fl., 5, 57–59, 1984.
</mixed-citation></ref-html>
<ref-html id="bib1.bib3"><label>3</label><mixed-citation>
Ardon-Dryer, K., Huang, Y.-W., and Cziczo, D. J.: Laboratory studies of collection efficiency of sub-micrometer aerosol particles by cloud droplets on a single-droplet basis, Atmos. Chem. Phys., 15, 9159–9171, <a href="https://doi.org/10.5194/acp-15-9159-2015" target="_blank">https://doi.org/10.5194/acp-15-9159-2015</a>, 2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib4"><label>4</label><mixed-citation>
Beard, K. V.: Terminal velocity and shape of cloud and precipitation drops
aloft, J. Atmos. Sci., 33, 851–864, 1976.
</mixed-citation></ref-html>
<ref-html id="bib1.bib5"><label>5</label><mixed-citation>
Beard, K. V. and Pruppacher, H. R.: A wind tunnel investigation of the rate
of evaporation of small water drops falling at terminal velocity in
air, J. Atmos. Sci., 28, 1455–1464, <a href="https://doi.org/10.1175/1520-0469(1971)028&lt;1455:AWTIOT&gt;2.0.CO;2" target="_blank">https://doi.org/10.1175/1520-0469(1971)028&lt;1455:AWTIOT&gt;2.0.CO;2</a>, 1971.
</mixed-citation></ref-html>
<ref-html id="bib1.bib6"><label>6</label><mixed-citation>
Bell, M. L., Davis, D. L., and Fletcher, T.: A retrospective assessment of
mortality from the London smog episode of 1952: the role of influenza and
pollution, Environ. Health Persp., 112, 6–8, 2004.
</mixed-citation></ref-html>
<ref-html id="bib1.bib7"><label>7</label><mixed-citation>
Brock, J. R.: On the theory of thermal forces acting on aerosol
particles, J. Coll. Sci. Imp. U. Tok., 17, 768–780, 1962.
</mixed-citation></ref-html>
<ref-html id="bib1.bib8"><label>8</label><mixed-citation>
Dépée, A., Lemaitre, P., Gelain, T., Mathieu, A., Monier, M., and
Flossmann, A.: Theoretical study of aerosol particle electroscavenging by
clouds, J. Aerosol Sci., 135, 1–20, 2019.
</mixed-citation></ref-html>
<ref-html id="bib1.bib9"><label>9</label><mixed-citation>
Dépée, A., Lemaitre, P., Gelain, T., Monier, M., and Flossmann, A.: Laboratory study of the collection efficiency of submicron aerosol particles
by cloud droplets – Part II:  Influence of electric charges, Atmos. Chem. Phys., 21, 6963–6984,
<a href="https://doi.org/10.5194/acp-21-6963-2021" target="_blank">https://doi.org/10.5194/acp-21-6963-2021</a>, 2021.
</mixed-citation></ref-html>
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Devell, L., Tovedal, H., Bergström, U., Appelgren, A., Chyssler, J., and
Andersson, L.: Initial observations of fallout from the reactor accident at
Chernobyl, Nature, 321, 192–193, 1986.
</mixed-citation></ref-html>
<ref-html id="bib1.bib11"><label>11</label><mixed-citation>
Dockery, D. W., Schwartz, J., and Spengler, J. D.: Air pollution and daily
mortality: associations with particulates and acid aerosols, Environ. Res.,
59, 362–373, 1992.
</mixed-citation></ref-html>
<ref-html id="bib1.bib12"><label>12</label><mixed-citation>
Flossmann, A. I.: Interaction of aerosol particles and clouds, J. Atmos. Sci., 55, 879–887, 1998.
</mixed-citation></ref-html>
<ref-html id="bib1.bib13"><label>13</label><mixed-citation>
Flossmann, A. I., Hall, W. D., and Pruppacher, H. R.: A theoretical study of
the wet removal of atmospheric pollutants, Part I: The redistribution of
aerosol particles captured through nucleation and impaction scavenging by
growing cloud drops, J. Atmos. Sci., 42, 583–606, 1985.
</mixed-citation></ref-html>
<ref-html id="bib1.bib14"><label>14</label><mixed-citation>
Greenfield, S. M.: Rain scavenging of radioactive particulate matter from
the atmosphere, J. Meteorol., 14, 115–125, 1999.
</mixed-citation></ref-html>
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Jackson, J. D.: Classical electrodynamics, 3rd edition, Wiley &amp; Sons, New York, London, Sydney, 808, 1999.
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Jaenicke, R.: Chapter 1: Tropospheric aerosols, Aerosol-cloud-climate interactions, in: International Geophysics, Vol. 54, edited by: Hobbs, P. Academic Press, 1–31, <a href="https://doi.org/10.1016/S0074-6142(08)60210-7" target="_blank">https://doi.org/10.1016/S0074-6142(08)60210-7</a>, 1993.
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Jost, D. T., Gäggeler, H. W., Baltensperger, U., Zinder, B., and Haller,
P.: Chernobyl fallout in size-fractionated aerosol, Nature, 324,
22–23, 1986.
</mixed-citation></ref-html>
<ref-html id="bib1.bib18"><label>18</label><mixed-citation>
Kaneyasu, N., Ohashi, H., Suzuki, F., Okuda, T., and Ikemori, F.: Sulfate
aerosol as a potential transport medium of radiocesium from the Fukushima
nuclear accident, Environ. Sci. Technol., 46, 5720–5726, 2012.
</mixed-citation></ref-html>
<ref-html id="bib1.bib19"><label>19</label><mixed-citation>
Ladino, L., Stetzer, O., Hattendorf, B., Günther, D., Croft, B., and
Lohmann, U.: Experimental study of collection efficiencies between submicron
aerosols and cloud droplets, J. Atmos. Sci., 68, 1853–1864, 2011.
</mixed-citation></ref-html>
<ref-html id="bib1.bib20"><label>20</label><mixed-citation>
Laguionie, P., Roupsard, P., Maro, D., Solier, L., Rozet, M., Hébert,
D., and Connan, O.: Simultaneous quantification of the contributions of dry,
washout and rainout deposition to the total deposition of particle-bound 7Be
and 210Pb on an urban catchment area on a monthly scale, J. Aerosol Sci., 77, 67–84, 2014.
</mixed-citation></ref-html>
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Lira, I.: Evaluating the measurement uncertainty: fundamentals and practical guidance, in: institute of physics, series in measurement science and technology, Institute of Physics Publishing, Bristol and Philadelphia, 251, <a href="https://doi.org/10.1119/1.1522703" target="_blank">https://doi.org/10.1119/1.1522703</a>, 2002.
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Pöllänen, R., Valkama, I., and Toivonen, H.: Transport of
radioactive particles from the Chernobyl accident, Atmos. Environ., 31,
3575–3590, 1997.
</mixed-citation></ref-html>
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Pruppacher, H. R. and Klett, J. D.: Microphysics of Clouds and Precipitation, in Atmospheric and oceanographic Sciences Library, Kluwer Academic Press, Dordrecht/Boston/London, 954 pp., 1997.
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Quérel, A., Lemaitre, P., Monier, M., Porcheron, E., Flossmann, A. I., and Hervo, M.: An experiment to measure raindrop collection efficiencies: influence of rear capture, Atmos. Meas. Tech., 7, 1321–1330, <a href="https://doi.org/10.5194/amt-7-1321-2014" target="_blank">https://doi.org/10.5194/amt-7-1321-2014</a>, 2014.
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Reischl, G. P. W. W., John, W., and Devor, W.: Uniform electrical
charging of monodisperse aerosols, J. Aerosol Sci., 8, 55–65, 2014.
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Santachiara, G., Prodi, F., and Belosi, F.: A review of termo-and diffusio-phoresis in the atmospheric aerosol scavenging process, Part 1: Drop scavenging, 2, 148–158, <a href="https://doi.org/10.4236/acs.2012.22016" target="_blank">https://doi.org/10.4236/acs.2012.22016</a>, 2012.
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Sharp, D. H.: Overview of Rayleigh-taylor instability, No. LA-UR-83-2130,
CONF-8305110-2, Los Alamos National Lab., New Mexico, USA, 1983.

</mixed-citation></ref-html>
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Tao, W. K., Chen, J. P., Li, Z., Wang, C., and Zhang, C.: Impact of aerosols
on convective clouds and precipitation, Rev. Geophys., 50, 1–62, <a href="https://doi.org/10.1029/2011RG000369" target="_blank">https://doi.org/10.1029/2011RG000369</a>, 2012.
</mixed-citation></ref-html>
<ref-html id="bib1.bib30"><label>30</label><mixed-citation>
Tinsley, B. A. and Zhou, L.: Parameterization of aerosol scavenging due to
atmospheric ionization, J. Geophys. Res-Atmos., 120, 8389–8410,
2015.
</mixed-citation></ref-html>
<ref-html id="bib1.bib31"><label>31</label><mixed-citation>
Tinsley, B. A., Zhou, L., and Plemmons, A.: Changes in scavenging of
particles by droplets due to weak electrification in
clouds, Atmos. Res., 79, 266–295, 2006.
</mixed-citation></ref-html>
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Twomey, S.: Pollution and the planetary albedo, Atmos. Environ., 8, 1251–1256, 1974.
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<ref-html id="bib1.bib33"><label>33</label><mixed-citation>
Waldmann, L. and Schmitt, K. H.: Thermo-phoresis and diffusiophoresis of
aerosols, Aerosol Science, Academic Press, London, UK, 137–162, 1966.
</mixed-citation></ref-html>
<ref-html id="bib1.bib34"><label>34</label><mixed-citation>
Wang, P. K., Grover, S. N., and Pruppacher, H. R.: On the effect of electric
charges on the scavenging of aerosol particles by clouds and small
raindrops, J. Atmos. Sci., 35, 1735–1743, 1978.
</mixed-citation></ref-html>
<ref-html id="bib1.bib35"><label>35</label><mixed-citation>
Wiedensohler, A.: An approximation of the bipolar charge distribution for
particles in the submicron size range, J. Aerosol Sci., 19, 387–389,
1988.
</mixed-citation></ref-html>--></article>
