Articles | Volume 22, issue 5
Atmos. Chem. Phys., 22, 3017–3044, 2022
https://doi.org/10.5194/acp-22-3017-2022
Atmos. Chem. Phys., 22, 3017–3044, 2022
https://doi.org/10.5194/acp-22-3017-2022

Review article 07 Mar 2022

Review article | 07 Mar 2022

Single-particle Raman spectroscopy for studying physical and chemical processes of atmospheric particles

Single-particle Raman spectroscopy for studying physical and chemical processes of atmospheric particles
Zhancong Liang1, Yangxi Chu2, Masao Gen3, and Chak K. Chan1 Zhancong Liang et al.
  • 1School of Energy and Environment, City University of Hong Kong, Hong Kong, 999077, China
  • 2State Key Laboratory of Environmental Criteria and Risk Assessment, Chinese Research Academy of Environmental Sciences, Beijing, 100012, China
  • 3Faculty of Frontier Engineering, Institute of Science and Engineering, Kanazawa University, Kanazawa, 920-1192, Japan

Correspondence: Chak K. Chan (chak.k.chan@cityu.edu.hk)

Abstract

Atmospheric particles experience various physical and chemical processes and change their properties during their lifetime. Most studies on atmospheric particles, both in laboratory and field measurements, rely on analyzing an ensemble of particles. Because of different mixing states of individual particles, only average properties can be obtained from studies using ensembles of particles. To better understand the fate and environmental impacts of atmospheric particles, investigations on their properties and processes at a single-particle level are valuable. Among a wealth of analytic techniques, single-particle Raman spectroscopy provides an unambiguous characterization of individual particles under atmospheric pressure in a non-destructive and in situ manner. This paper comprehensively reviews the application of such a technique in the studies of atmospheric particles, including particle hygroscopicity, phase transition and separation, and solute–water interactions, particle pH, and multiphase reactions. Investigations on enhanced Raman spectroscopy and bioaerosols on a single-particle basis are also reviewed. For each application, we describe the principle and representative examples of studies. Finally, we present our views on future directions on both technique development and further applications of single-particle Raman spectroscopy in studying atmospheric particles.

1 Background

Atmospheric particles or aerosols have considerable effects on climate and human health (Seinfeld and Pandis, 2016). In general, atmospheric particles can originate from a wide variety of anthropogenic and natural sources. Primary particles are emitted directly as a liquid or solid (e.g., soot particles, mineral dust), and they can also undergo atmospheric multiphase reactions. Secondary particles can also be generated by gas-to-particle conversions, such as new particle formation via nucleation and condensation (Pöschl, 2005). During their atmospheric lifetime, both primary and secondary particles are subject to physical and chemical processes, such as partitioning and multiphase reactions. For liquid particles, gas–particle partitioning takes place to achieve thermodynamic equilibrium. For example, an increase or decrease in relative humidity (RH) would result in the uptake of the water vapor into deliquescent particles or the evaporation of particulate water to the gas phase, respectively. Multiphase reactions can be described as gas–particle partitioning accompanied by chemical reactions. Furthermore, photochemistry is an important group of multiphase reactions during the daytime. Both partitioning and chemical reactions can change the composition of the particles, altering their properties such as hygroscopicity, cloud condensation nuclei (CCN) activities, phase state, morphology, reactivity, toxicity, and, finally, environmental impacts.

Physical and chemical processes of atmospheric particles have been examined by numerous experimental approaches: a flowing stream of aerosol particles in an open system (flow tube) (Li et al., 2015; Duporté et al., 2017; Heine et al., 2018; Liu and Abbatt, 2020; T. Liu et al., 2020; Peng and Jimenez, 2020), a chamber of suspending particles (smog chamber) (Akimoto et al., 1979; Behnke et al., 1988; Liu et al., 2016; Ye et al., 2018; Charan et al., 2019; Liu and Abbatt, 2021; Qin et al., 2021), a collection of deposited particles (Bao et al., 2018; Y. Zhang et al., 2020), and single particles (Lee and Chan, 2007a; Krieger et al., 2012; Davies and Wilson, 2016; Gen et al., 2019c; Gong et al., 2019; Sullivan et al., 2020). An aerosol flow tube is one of the most common approaches employing a flowing stream of aerosol particles. It enables real-time characterization of reaction products and particulate size under controlled conditions (e.g., RH, temperature), with instruments connected to the exit or different outlets along the flow tube reactor. Oxidation flow reactors (OFRs) are analogous to the general aerosol flow tube, but photooxidants (e.g., OH radical) are introduced to examine secondary organic matter formation (Kang et al., 2007; Smith et al., 2009; George and Abbatt, 2010; Keller and Burtscher, 2012). Typically, higher concentrations of reactive precursor gases than ambient concentrations are used in these flow systems to compensate for the relatively short residential time (e.g., seconds) of the reactants. However, such equivalency of exposure may not necessarily hold (Lee and Chan, 2007b; Chu et al., 2019). Smog chambers enable simulations of various environmental conditions, including gas concentrations, for studying the formation and chemical transformation of particles. The residence time of particles can be extended to a few hours, but other limitations exist, such as long response time to control or change conditions, high cost, and wall loss of particles (Kang et al., 2007). Deposited particles can be studied using a sample-loaded substrate/filter placed in a flowing-gas reactor or a flow tube with its internal wall coated with particles. Environmental conditions can be easily varied, and the reaction time can be very long. An in situ analyzer for spectroscopic analysis can be equipped (e.g., Raman, Fourier transform infrared spectrometry (FTIR)) since the particles are immobilized on a substrate/filter. However, a large number of particles or large particles are usually required to achieve sensitive detection. The influence of particle loading on the reactions and chemical characterization is a challenging question. In general, these approaches produce statistical results of a collection of particles. They may not truly reflect the interaction between gas and particle since the composition of the individual particles may not be identical (Ault and Axson, 2017).

Single-particle characterization has the advantage that the physical and chemical processes undertaken by the particle can be unambiguously monitored. While there is a wealth of instruments for comprehensively characterizing single particles, some are destructive (e.g., mass spectroscopy) or operate under vacuum conditions (e.g., electron microscopy), making them unsuitable for monitoring the gas–particle interaction on the same particles. Single-particle spectroscopic methods (e.g., Raman) can be good alternatives, but the particles are usually supermicron and up to tens of microns. The findings from particles much larger than ambient ones need to be interpreted carefully for drawing implications in submicron atmospheric particles.

Despite its requirements of relatively large particles for spectroscopic signals, single-particle Raman spectroscopy offers several advantages for studying atmospheric processing of aerosol particles. First of all, a single particle can be unambiguously characterized in situ without destruction. From the Raman spectra, chemical compositions of typical aerosol particles (i.e., soot, sulfate, organics, etc.) can be identified by their characteristic peaks. Interactions between molecules can be inferred by peak shifts and changes in peak width. Particulate properties such as the phase state and size can also be characterized by coupling levitation (or isolation) technique and optical microscopy. We will elaborate on the applications of these functions later.

Furthermore, Raman analysis is operated under atmospheric pressure and enables the use of atmospherically relevant concentrations for a long exposure time to examine atmospheric gas–particle interactions (Lee and Chan, 2007a). Micro-Raman systems can provide spatial information of chemical species at 2-D or even 3-D levels (Batonneau et al., 2006; Sobanska et al., 2006, 2014, 2015; Tripathi et al., 2009; Scolaro et al., 2009; Offroy et al., 2015; Falgayrac et al., 2018; Ao et al., 2020). Recent advances in stimulated Raman scattering by micro-Raman spectroscopy further improve the spatial resolution from 1 µm to 350 nm and significantly shorten the scanning time from 2.5 h to 2 s (Ao et al., 2020). The disadvantage of Raman spectroscopy is that it can only detect Raman-active functional groups but cannot provide information on the exact molecular structures. Light-absorbing chemicals such as humic-like substances (HULIS) or some brown carbon species may generate fluorescence, interfering with the peak identification in the spectra (Ivleva et al., 2007a). Therefore, single-particle Raman spectroscopy is more suited for laboratory-generated particles than ambient particles. FTIR does not suffer from fluorescence since it uses a longer wavelength (up to tens of µm), but the long wavelength also lowers the spectral resolution (Ault and Axson, 2017). Also, Raman scattering has advantages over FTIR for water-containing samples because the strong water peaks in the latter can mask the peaks from other components or even make them undetectable (Nishikida et al., 2018).

This paper will introduce the general setup of the single-particle Raman spectrometer, how single particles can be characterized unambiguously, and examples of physical and chemical processes reported in the literature. We focus on applications of atmospheric relevance and refer readers to other literature on the principles of Raman spectroscopy and related techniques (e.g., stimulated Raman or coherent anti-Stokes Raman spectroscopy) and applications of less direct atmospheric relevance (Tolles et al., 1977; Efremov et al., 2008; Jones et al., 2019). Finally, we will provide suggestions on future directions of Raman spectroscopy for atmospheric particle studies.

2 General setup of single-particle Raman spectroscopy

2.1 Particle isolation

In general, single-particle Raman spectroscopy consists of two key components: particle isolation and Raman spectroscopy, including micro-Raman and confocal Raman configurations. One of the most popular approaches for single-particle isolation is particle levitation, which has been discussed in a few reviews (Reid and Mitchem, 2006; Mitchem and Reid, 2008; Krieger et al., 2012). In this paper, we will briefly introduce their principles and configurations and focus on atmospheric applications. Techniques for levitation of particles can be mainly divided into electrical, optical, and acoustic trapping. Another approach for particle isolation is particle deposition onto substrates with Raman analyses of single particles on an individual basis.

2.1.1 Electrodynamic balance

The electrodynamic balance (EDB) has been used for studying single particles with a diameter of 1–100 µm since the 1980s (Davis and Ray, 1980). A particle is levitated and trapped at the null point under the alternating current (AC) and direct current (DC) electric fields in the EDB. In the absence of other forces, the gravitational force of the particle trapped in the EDB is equal to the balancing electrostatic force, as shown in Eq. (1):

(1) m g = n q C V DC z ,

where m is the mass of the particle, g is the gravitational constant, n is the number of elementary charges present on the particle, q is the elementary charge, z is the distance between two electrodes for the DC voltage, C is a constant dependent on the geometrical configuration of the EDB, and VDC is the balancing DC voltage required to levitate the particle stationary. According to Eq. (1), the mass of the particle is proportional to the DC voltage needed to balance its gravitational force, assuming that the charge present on the trapped particle remains constant. Hence, the relative mass change in the particle undergoing any physical or chemical processing can be quantified by measuring the balancing DC voltage. With a levitated particle stationary, Raman spectroscopy of the stably trapped particles can provide chemical information. Coupled with mass change measurements and optical microscopy, physical and chemical characterization of single particles can be in situ monitored. In addition to the traditional single-particle EDB (Davis and Ray, 1980; Chan et al., 1992), other EDB setups, for example, quadrupole (Q)-EDB and comparative kinetic (CK)-EDB, have been developed. Q-EDB allows the trapping of multiple droplets simultaneously. During chemical reactions, individual particles are released one at a time for mass spectroscopy analysis, while the rest of the particles are kept levitated for in situ spectroscopic characterization (Singh et al., 2017, 2018; Jacobs et al., 2017; Kohli and Davies, 2021). CK-EDB employs a reference droplet with known composition and hygroscopic property, which serves as an accurate probe for the environmental conditions in which the tested droplet is examined. It affords hygroscopicity measurements and mass-transfer kinetic measurements on the droplets at high RH (>99 %) (Davies et al., 2013; Rovelli et al., 2016; Marsh et al., 2019).

2.1.2 Optical trapping

Optically traps can be basically categorized into radiation pressure trap, photophoretic trap, and universal optical trap. Radiation pressure trap, which is the most general in studying aerosol particles, utilizes the radiation pressure from a light source to balance the weight of the levitated particle (Ashkin, 1970). During optical trapping, the particle interacts with a highly focused laser beam and experiences scattering and gradient forces (Ashkin and Dziedzic, 1981; Mitchem and Reid, 2008). The scattering force is proportional to the square of the induced dipoles and the intensity of the incident laser beam, acting as a force along the direction of the beam propagation. In contrast, the gradient force derives from the focusing of the laser beam and draws the particle towards the region with the highest light intensity (Krieger et al., 2012).

Radiation pressure-based optical levitation and optical tweezers are two typical optical-trapping techniques utilizing these two forces. While optical levitation relies on the exact balance between downward gravitational force and upward scattering force, optical tweezers effectively create a strong intensity gradient in three dimensions by tightening the focus of the laser beam to generate amplified gradient forces. Optical tweezers provide a more robust trap with the gradient force typically many orders of magnitude larger than the scattering and gravitational forces, leading to three-dimensional confinement in position with a single laser beam. However, particle size changes must be accompanied by dynamic changes in the light intensity for retaining the trapped particle. In principle, transparent non-absorbing particles of 1–100 µm in diameter can be trapped with dynamic light intensity adjustment for droplet size changes. By configuring a Bessel laser beam, instead of the typical Gaussian beam, in either vertically or horizontally trapping arrangements, optical levitation and tweezers can be applied for trapping submicron particles (Meresman et al., 2009; Cotterell et al., 2014; Lu et al., 2014). However, Raman spectroscopy would require larger particles for sufficient signal-to-noise ratios. A recent study reported a photochemical study of aerosol particles using an optical trap for the first time by employing a custom-built photochemical levitation chamber (Gómez Castaño et al., 2019). A sidewall of the chamber is equipped with quartz windows for a UV lamp.

In addition to radiation pressure traps, photophoretic traps and universal optical traps are two emerging alternatives (Redding et al., 2015a; Redding and Pan, 2015). The former is specifically for light-absorbing particles. The latter employs a hollow beam to trap transparent and light-absorbing particles using radiation pressure force and photophoretic force, respectively (Gong et al., 2018a). Using these techniques, Raman characterizations have been made on light-absorbing particles in recent years, including bioaerosols (C. Wang et al., 2015; Redding et al., 2015a, b; Gong et al., 2018b, 2019), aromatic compounds (Kalume et al., 2017a, b; Gong et al., 2018b), carbon nanotubes (Pan et al., 2012; Gong et al., 2018b), and soot (Uraoka et al., 2017).

2.1.3 Acoustic levitation

Compared to the EDB and optical trap, acoustic levitation is less utilized in atmospheric research due to the complicated acoustic streaming and the requirement for large particles (20 µm–2 mm) (Cohen et al., 2020; Jones et al., 2021). In an acoustic levitator, high-frequency sound waves generated by a piezo-electric radiator reflect from a concave-shaped reflector to generate a standing wave. The latter produces acoustic radiation pressure on the particle, levitating and trapping it against the gravitational force. It has been reported that a single particle can be firmly trapped by acoustic levitation under 15 h continuous irradiation (Tobon et al., 2017; Seng et al., 2018).

2.1.4 Deposited particles

In addition to single-particle levitation, deposited particles on a surface provide a convenient platform for single-particle Raman spectroscopy. While levitation can trap few particles for investigation, surface-based isolation affords a relatively large number of single particles, which can support further offline characterizations. However, the direct contact between particle and substrate may induce solute nucleation or phase separation that causes unexpected modification in particulate morphology. Hence, hydrophobic substrates are often used to study supersaturated aqueous droplets by reducing the particle and substrate contact area. Investigations on photochemistry can be easily performed by coupling a transparent substrate and an additional light source beneath the quartz window at a flow cell's bottom (Gen et al., 2019c, 2020). A single particle can be retained for an infinite time deposited, facilitating studies of slow processes in the atmosphere. However, Raman scattering from the substrate could also show interference.

2.2 Raman spectroscopy

A single-particle Raman spectroscopy setup generally involves a laser for excitation, followed by collection optics to detect the Raman signals analyzed by a spectrometer with a monochromator and a charge-coupled device (CCD) detector. The Raman peak location and intensity/area provide information on the speciation and abundance of specific particulate components. Appendix A summarizes the Raman peak assignment of representative atmospheric species. A Raman peak can also shift its location (in wavenumber) and change in the full width at half maxima (FWHM) as a response to variations of local bonding environments, such as molecular interaction and phase transition. Furthermore, Raman emissions from spherical particles (e.g., levitated droplets) can be complicated by resonance modes at discrete wavelengths triggered by cavity-enhanced Raman scattering (CERS) (Miles et al., 2012) or so-called size parameters in the spectra. These resonant modes are often called morphology-dependent resonance (MDR) or whispering gallery modes (WGMs) (Chan et al., 1991; Krieger et al., 2012). They can be used to accurately determine size with a resolution down to ∼5 nm, refractive index, and even shell–core morphology of the mixed organic–inorganic particles based on the Mie theory (Gorkowski et al., 2017, 2020; Rafferty and Preston, 2018; Sullivan et al., 2020). The optical effects complicate the Raman measurements for chemical analysis, although they provide additional information for the sizing and refractive index of the particles based on Mie theory. We refer readers to the references for the interactions between Mie scattering and Raman spectroscopy (Chan et al., 1991; Krieger et al., 2012; Nadler et al., 2019). Micro-Raman is a combined system that uses an optical microscope for guiding the laser to analyte particles and collect Raman scattering from the same microscope connected to a spectrometer. The Raman scattering signal-to-noise ratio can be enhanced since the incident laser energy is focused on a small volume through a high magnification (and short working distance) objective. Furthermore, 2-D Raman imaging is possible in studying particles in the order of tens of microns (Eom et al., 2016; Zhao et al., 2018). Confocal Raman micro-spectroscopy eliminates the Raman scattering from volumes other than the focal volume by configuring additional slits in the spectrometer. Confocal Raman provides depth profiles of constituent information of the particle (Scolaro et al., 2009).

This paper focuses on the use of single-particle Raman spectroscopy to examine the physical and chemical processes of atmospheric particles. We describe techniques of particle maneuvering that allow single-particle Raman spectroscopy such as EDB, deposited particles, and optical trapping. However, it is not our intention to conduct a detailed examination of the application of these techniques beyond single-particle Raman spectroscopy. Hence, in this review, we put less emphasis on literature related to other applications of these trapping techniques. We focus on investigating these physical and chemical processes of particles by Raman instead of the particle properties or detailed descriptions of these processes investigated by other techniques. The overall aim of the paper is to introduce single-particle Raman spectroscopy as a useful tool to examine a host of processes of atmospheric relevance.

3 Characterization of single particles

3.1 Hygroscopicity and phase transition

Depending on the environmental RH, type of solutes, and size of the particles (Kelvin effect), atmospheric particles can absorb/release an appropriate amount of water to reach equilibrium with the gas phase; i.e., the partial water vapor pressure above the particle surface equals to that of the gas phase. Hygroscopic properties include water uptake/evaporation and phase transition as a response to changes in ambient RH. Upon water uptake/evaporation, the particle size change alters the particulate capacity in scattering light, and particles can also be activated to cloud condensation nuclei (Tang et al., 2019). In this paper, we focus on subsaturated (RH <100 %) environments. The phase states determine the water uptake behaviors of the atmospheric particles (Pajunoja et al., 2016; Rosati et al., 2020). They can be generally divided into liquid (i.e., aqueous), crystalline, and amorphous (e.g., ultra-viscous, gel, rubber, glasses). Both crystalline and amorphous particles are solids, but only the latter can absorb water reversibly, while the former shows hysteresis in water uptake. At increasing RH, water uptake increases the aerosol liquid water (ALW) content of deliquescent/amorphous particles and their size and ability to scatter light. A recent study showed that the poor visibility during haze in the North China Plain is positively correlated to the ALW (Z. Wu et al., 2018). When crystalline particles are exposed to increasing RH, they will initially adsorb a small amount of water on its surface, the so-called surface-adsorbed water (SAW), and then uptake a significant amount of water vapor abruptly to become aqueous droplets at the deliquescence RH (DRH). The DRH is the RH at which a droplet attains the saturated salt concentration, ignoring the influence of the Kelvin effect, which is often the case for single-particle Raman analysis (particle size >10µm). At decreasing RH, a droplet loses water to become supersaturated and finally may effloresce to form crystalline particles at the efflorescence RH (ERH). Typical inorganic atmospheric components of (NH4)2SO4, NH4NO3, and NaCl deliquesce at ∼80 %, ∼62 %, and ∼75 % RH but effloresce at 34 %–48 %, 0 %–30 %, and 39 %–54 %, respectively. Many studies show that nitrates and some organics do not effloresce even at low RH (e.g., below 5 %) (Mikhailov et al., 2009; Yeung and Chan, 2010). In general, organics with high solubility (e.g., malonic acid) tend to remain a supersaturated liquid state or amorphous state at low RH (Krieger et al., 2012). Unlike DRH, which is thermodynamically well defined, ERH is a stochastic property that relates to the kinetics of nucleation and presence of impurities. It has been reported that sucrose crystals deliquesce at 85.6 % RH upon humidification, but the aqueous droplets turn into a glassy amorphous state upon drying instead of forming crystallized solids (Zobrist et al., 2011). Using EDB and optical trap experiments, hygroscopic changes and phase transition RH values that involve rapid changes in mass or size can be measured by the balancing voltage and light scattering, respectively. The growth factor (GF) in terms of mass or size ratios as a function of water activity or RH, DRH, and ERH can be easily determined by changes in mass or size and the light-scattering pattern (Chan et al., 2005; Mitchem et al., 2006; Marsh et al., 2017).

While GF, DRH, and ERH measurements are readily made for mixed particles using EDB and optical traps, the formation of mixed-phase particles before full deliquescence is more complicated. For example, unlike the corresponding single inorganic salts, NaCl-malonic acid and (NH4)2SO4-malonic acid mixed particles absorb a significant amount of water before their DRH since malonic acid absorbs water reversibly without crystallization (Lee et al., 2008a). However, these stepwise water uptake and phase transition behaviors could not be explained by EDB/optical levitation mass or size measurements alone, due to the lack of chemical characterization. Raman spectroscopy offers complementary information on the water uptake behaviors and phase states of Raman-active species (Yeung and Chan, 2010; Li et al., 2017). For example, the water-to-solute ratio (WSR) as a function of ambient RH can be easily determined from the integrated peak area ratio of the water v(O−H) to that of the solute (e.g., sulfate, nitrate) after proper calibration. Also, the full width at half maxima (FWHM) of the characteristic peaks is sensitive to the phase state of the solute. In general, a species in the liquid phase has a larger FWHM than in the solid phase because the less compact molecular arrangement allows minor variations in vibration. In Fig. 1a and b, as the RH decreased to 39.5 % for ammonium sulfate (AS) and 19 % for ammonium nitrate (AN), crystallization can be inferred by the red shift and decrease in FWHM of sulfate and nitrate peaks, as well as the disappearance of water peak. On this basis, the mixed-phase particle prior to full deliquescence can be characterized by FWHM of different Raman-active components. For instance, Ling and Chan found an increased FWHM of nitrate peak (∼730 cm−1) at ∼67 % RH, followed by an increased FWHM of sulfate peak (∼450 cm−1) at ∼76 RH % for mixed-phase AS–AN particles when RH increased (Fig. 1c, d). These changes indicate that AN deliquesced before AS did upon humidification, and the mixed-phase AS–AN particle was composed mainly of aqueous AN and crystalline AS. The accuracy of single-particle Raman spectroscopy in determining hygroscopicity has been verified by thermodynamic models such as E-AIM and UNIFAC (Peng et al., 2001; Yeung and Chan, 2010). There are numerous hygroscopicity applications on various specific systems, including model inorganics, organics, and their mixtures (Chu et al., 2015; Laskina et al., 2015; W. Wang et al., 2021; Tobon et al., 2021; C. Zhang et al., 2021; Ashraf et al., 2021), as well as mineral dust (Liu et al., 2008), secondary organic aerosols (Wu et al., 2020), and atmospherically relevant biological macromolecules (Mael et al., 2021), using single-particle Raman spectroscopy. It should be noted that evaporation of some components and precipitation of some salts could occur during the RH cycling in hygroscopicity measurements (Li et al., 2017, 2021; Cai and Zhao, 2018; Ma et al., 2019a, b; Wu et al., 2020). Single-particle Raman spectroscopy can probe such processes in situ by the disappearance of some characteristic peaks (evaporation) or changes in their FWHM (precipitation) (Braban et al., 2003; Wang et al., 2017).

https://acp.copernicus.org/articles/22/3017/2022/acp-22-3017-2022-f01

Figure 1Raman spectra of a single (a) AS and (b) AN particle upon evaporation (Yeung and Chan, 2010). FWHM of (c) SO42- peak and (d) NO3- peak during the evaporation–growth cycle of a mixed AS–AN particle.

3.2 Solid-phase transition

In addition to liquid–solid-phase changes, transitions can occur between solid phases, from a metastable one to a stable one at a specific temperature. Many organics are known to form polymorphs, defined as solids with the same chemical composition but distinctive properties such as thermal stability and solubility due to different structures (Krieger et al., 2012). Different polymorphs of the same compound can exhibit different Raman characteristics, which can identify different solid states and their transition. For example, crystalline glutaric acid (GA) particles could exist as the metastable α-form and the thermodynamically stable β-form at room temperature, and α-form GA tends to transfer into β-form. Using EDB–Raman spectroscopy, Chan et al. (2006) coated GA on AS particles by coagulation of small GA particles formed by nucleation. Raman spectra showed the existence of α-form GA in the freshly coated particles, but then the β-form was detected after a deliquescence–crystallization cycle (Chan et al., 2006). Ling and Chan (2008) reported the formation of the α-form GA solid in a freshly crystallized GA–AS particle. The α-form GA solid gradually transformed to the β-form at 60 % RH in 3 h at room temperature (Ling and Chan, 2008). Furthermore, Yeung et al. (2010) examined the effects of polymorphism on the hygroscopic properties of GA particles using micro-Raman (Yeung et al., 2010). By evaporation at room temperature, α-form and β-form solid particles were formed (α:β5:1). It was observed that the α-form deliquesced at 85 %–86 % RH, whereas the β-form deliquesced at 90 % RH. Furthermore, the α-form is transformed to the β-form at 86 % RH instead of achieving full deliquescence (Fig. 2). This solid-phase transition behavior was used to explain the discrepancies of DRH values of glutaric acid particles reported based on different literature measurements (Cruz and Pandis, 2000; Peng et al., 2001; Choi and Chan, 2002; Parsons et al., 2004; Zardini et al., 2008; Treuel et al., 2009). Polymorphism also exists in atmospherically relevant inorganics. For example, AN can exist in five stable polymorphic forms with distinct Raman spectra, depending on the temperature. In atmospheric research, very little attention has been paid to the solid-phase transitions of AN because phase IV AN particle is stable over a wide range of tropospheric temperatures (from 17 to 32 C) (Wu et al., 2007). Nevertheless, Wu and Chan (2008) reported that the KNO3/AN mixed particles undergo the IV–III transition under ambient temperatures at a relatively high mass percentage of KNO3(≥7.4 wt %) or even crystallize directly in phase III from droplets with a further increase in the mass percentage of KNO3 (Wu and Chan, 2008).

https://acp.copernicus.org/articles/22/3017/2022/acp-22-3017-2022-f02

Figure 2Raman spectra of deliquescent α-glutaric acid, crystalline α-glutaric acid, and β-glutaric acid (Ling and Chan, 2007).

Another typical solid-phase transition is between stable and metastable double salts. Like metastable/stable polymorphs, metastable double salts show Raman characteristics different from stable ones, likely due to specific molecular interactions. Ling and Chan (2007) observed the double-salt 3AN  AS, not predicted from thermodynamics, in the freshly crystallized mixed single particles of AN and AS using single-particle Raman spectroscopy (Ling and Chan, 2007). The existence of double salts indicates that AN and AS likely crystallized simultaneously. The degree of metastability could depend upon the crystallization processes of the particles. Besides, it takes several hours to more than a day, depending on RH, for a freshly crystallized metastable AS–AN double-salt particle to reach its stable form, suggesting a high possibility that metastable solids persist in the atmosphere when the ambient RH is sufficiently low. The AN–AS double salts were recently reported in ambient particles in Beijing (Sun et al., 2019b; M. Wang et al., 2021).

3.3 Molecular interactions between particulate water and solutes

In general, characterizations on phase transitions rely on the sensitivity of Raman spectroscopy in probing the bonding environment of components in the particles. Raman spectroscopy can also characterize the interactions between the solutes and particulate water, such as hydrogen/ionic bonding. For example, the Raman shift of strongly hydrogen-bonded water (∼3500 cm−1) is generally higher than that of water monomers (∼3300 cm−1) (Zhang and Chan, 2003). At low RH, the elevated concentration of electrolytes leads to more significant disruption of the hydrogen bonding environment of the water molecules, resulting in a shift of OH stretching peak at 3480 cm−1 to higher frequencies. In contrast, the low-frequency shoulder at 3290 cm−1 diminishes. Thus, the shape of water peaks in Raman spectra can reflect the ionic strength of the particle, which is an essential parameter for aerosol chemistry (Mitchem et al., 2006; Mekic et al., 2020). The sensitive shift of water peak has also been used in studying ice nucleation properties such as depositional freezing (Wise et al., 2010, 2012) and immersing freezing (Knopf et al., 2002, 2003). Specifically, while liquid water peaks are usually located at ∼3400 cm−1 with a shoulder at a lower wavenumber, a sharp peak at ∼3150 cm−1 with shoulder peaks at ∼3200 cm−1 appears as water is frozen (Schill et al., 2014; Mael et al., 2019). Besides, ionic bonding of inorganic salts (e.g., SO42-, NO3-) can also be reflected by their Raman characteristics; and many of them have been further supported by theoretical calculations (Yu et al., 2012; Y. Wang et al., 2015; Zhu et al., 2018). For example, Zhang and Chan (2000) observed a blue shift of sulfate and nitrate Raman peaks and an increase in FWHM when the molar water to the solute ratio (WSR) in MgSO4 and Mg(NO3)2 particles decreases to less than six, the number of hydration of Mg2+ ions (Zhang and Chan, 2000; Zhang et al., 2004). These observations were attributed to direct contacting ion pairs formed between Mg2+ and anions, without water molecules between the ions. Besides, single-particle Raman spectroscopic analysis can reveal the structural heterogeneity of droplets. Raman imaging suggested that the NO3- to Mg2+ ratio of the contact ion pairs increases but the H2O to Mg2+ ratio decreases as the surface of a highly supersaturated droplet is approached (Zhang et al., 2004). Yeung and Chan (2010) reported that though no crystallization was shown by glyoxylic acid particle even at 0 % RH, a new C=O peak at ∼1820 cm−1 appeared together with the aqueous C=O peak at 1735 cm−1, possibly indicating the presence of anhydrate (Yeung and Chan, 2010).

3.4 Liquid–liquid phase separation

As mentioned above, partial crystallization can lead to a separation of solid and liquid mixed phases. Separation of two or even more liquid phases, namely liquid–liquid phase separation (LLPS), is also possible (Song et al., 2012a, 2018; Y. Huang et al., 2021; Ma et al., 2021). LLPS can be triggered by the interactions between inorganic and organic solutes and particulate water in mixed particles (You et al., 2012; Renbaum-Wolff et al., 2016). This phenomenon is mainly attributed to the low solubility of some non-polar or weakly polar organics, especially in the presence of inorganic salts, which may further decrease the solubilities of organics as the salting-out effects (Setschenow, 1889).

Optical microscopy (as a part of a single-particle Raman microscope) can directly indicate LLPS by the contrasting colors on appearance, based on the different refractive indices of materials in different phases (You et al., 2012). Single-particle (micro-)Raman spectroscopy can examine LLPS via spatial scanning (micro-Raman), optical imaging (micro-Raman), Raman imaging, and whisper gallery modes (WGMs) with additional chemical information of the different phases (Bertram et al., 2011; Song et al., 2012b). Spatial scanning records distinct micro-Raman spectra at different locations of the particle and reveals LLPS (Bertram et al., 2011; F. M. Wu et al., 2018) such as core–shell structures (e.g., an aqueous core surrounded by a BC-containing organic shell) (Brunamonti et al., 2015). However, Raman spatial scanning requires accurate focusing of the laser onto different targeted phases, which can be difficult when phases are separated into multiple small inclusions (Buajarern et al., 2007b).

Using spatial scanning and optical imaging, Ma et al. (2021) reported an organic-shell–aqueous-core LLPS in deposited 1,2,6-hexanetriol / ammonium sulfate mixed particles. However, different substrates for deposited particles could affect their LLPS behavior (Ma et al., 2021). Though LLPS of an organic / AS mixed particle has been observed on both hydrophobic (i.e., PTFE) and hydrophilic (i.e., glass) substrates, the former shows an organic shell with an AS inner core while the latter shows an opposite configuration (Q. Zhou et al., 2014). To eliminate interaction with substrates, Ishizaka et al. (2021) used levitated droplets and found both core–shell and partially engulfed LLPS. The observed configurations of two phases are well consistent with thermodynamic predictions based on interfacial tensions and relative volume ratios of two immiscible phases (Ishizaka et al., 2021).

Another approach for identifying LLPS is Raman imaging of the whole particle in one single measurement. Typical Raman measurements bin the vertical pixels of a CCD to enhance the signa-to-noise ratio, while the horizontal pixels represent the wave number after chromatic dispersion by a grating. Zhang et al. (2004) used collection optics to obtain an image of a particle in an EDB on the slit of a monochromator. Instead of using vertical binning, the vertical pixels registered the vertical profile of the Raman scattering (e.g., edge to center to edge) of the particle (Zhang et al., 2004). Chu and Chan (2017b) reported that the core–shell phase separation in a mixed sucrose–ammonium-sulfate particle with a sucrose molar fraction of 50 % at <5 % RH but not at 70 % RH. As shown in Fig. 3a and b (<5 % RH), the accumulated C−H signal on the two sides indicates the presence of an organic-rich coating and an organic-deficient core. In contrast, the even distribution of the C−H signal in Fig. 3c (70 % RH) suggests that the particle is likely homogeneous (Chu and Chan, 2017b). Kalume et al. (2018) observed temporally resolved LLPS in a diethyl phthalate and glycerol mixed droplet. Upon evaporation, diethyl phthalate migrated to the surface and formed an outer layer, and glycerol was more concentrated in the interior of the droplet (Kalume et al., 2018).

https://acp.copernicus.org/articles/22/3017/2022/acp-22-3017-2022-f03

Figure 3Spatially resolved Raman intensities of AS–sucrose (molar fraction of sucrose in total solute (FSU=0.5)) particles equilibrated at <5 % RH for 2 h (a) and for 11 h (b) and at 70 % RH for 2 h (c). C−H peaks at ∼2900 cm−1 represent sucrose. Solid lines indicate the particle's upper and lower edges. The outer regions between the dashed and solid lines are sucrose-rich in panels (a)(b) (Chu and Chan, 2017b).

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Additionally, WGMs have also been utilized to infer the occurrence of LLPS and the specific particle morphologies. For example, different resonance structures appear in the Raman spectra when core–shell or engulfed phase separation occur (Buajarern et al., 2007a, b; Kwamena et al., 2010; Song et al., 2013; Marcolli and Krieger, 2020). Sharps peaks generated by WGMs in spectra can be found if the spatial distribution of particulate species is symmetric, such as those in core–shell separated and homogeneously mixed particles, though the number, location, and intensity of WGMs peaks are different. In contrast, the engulfed phase-separated particles do not show any WGMs peaks (Sullivan et al., 2020). Utilizing WGMs, Steward et al. (2015) reported the transition between partially engulfed and core–shell structure at different RH values (Stewart et al., 2015). However, these analyses focus on WGMs but not Raman as a chemical probing technique.

3.5 Determination of pH

The pH, defined as the activity of proton in aerosol particles, can also be inferred from Raman spectra based on the intensity of the conjugate acid–base ion pairs. Sulfate/bisulfate has been used most frequently. The pH can be determined by substituting the conjugate ion pair concentrations and its dissociation coefficient into Henderson–Hasselbalch (H−H) (Radić and Prkić, 2012), Debye-Hückel theory, and specific ion interaction theory equations, respectively (Ciavatta, 1980; Rindelaub et al., 2016; Craig et al., 2017, 2018; Coddens et al., 2019; Chang et al., 2020a). The latter two are more suitable to supersaturated particles since non-ideality has been considered. Rindelaub et al. (2016) reported direct measurements of pH in individual deposited particles according to sulfate/bisulfate peaks in Raman spectra and its variation with RH (Rindelaub et al., 2016). Craig et al. (2017) extended this approach to a range of atmospherically relevant inorganic and organic acid–base equilibria systems covering a wide range of pH (from 1 to 10) (Craig et al., 2017). To eliminate the artifact of contacts between the particle and the substrate, Coddens et al. (2019) determined the pH of trapped particles via titration by coalescence of droplets containing strong acids (Coddens et al., 2019). Boyer et al. (2020) further utilized the WGMs for determining the solute concentration in real time and achieved uncertainties in pH measurements of picoliter droplets ranging from ±0.03 to 0.06 pH units (Boyer et al., 2020). Very recently, Cui et al. (2021) reported that water can be used to probe pH in individual model aerosol particles (e.g., (NH4)2SO4, NaCl), since the water bands are affected by other components (e.g., ions), as discussed in Sect. 3.3. Specifically, the broad water peak at 2600–3800 cm−1 could comprise many overlapping peaks, representing O−H vibration of water molecules in different local environments. The addition of solutes affects the local environment of water molecules and changes the relative intensities of the overlapped peaks. Hence, the activity of specific solutes can be obtained by analyzing the overlapped water peaks after rigorous calibration, and the pH of the aerosol particle can be calculated (Cui et al., 2021).

4 Multiphase reactions

In Sect. 3, applications of characterizing single particles have been reviewed. This section mainly focuses on the processes occurring on single particles. Taking water-solute interactions as an example, hygroscopicity describes the ability of solutes to absorb water upon equilibrium at fixed RH. Water uptake is a dynamic process, although it is generally too quick to be a limiting step in most atmospheric applications. However, in some viscous matrixes, the water uptake rate could be reduced by orders of magnitude due to the limited diffusion (Chang et al., 2020b). Taking advantage of the different Raman characteristics of D2O and H2O, Davies and Wilson (2016) measured the diffusion coefficients of water molecules in trapped viscous particles by monitoring the isotopic exchange rate using Raman spectroscopy (Davies and Wilson, 2016). Determination of kinetic parameters of non-reactive processes such as partitioning coefficient, diffusion coefficient, and mass accommodation coefficient has been reviewed in another paper (Krieger et al., 2012). Hence, applications on probing multiphase reactions using single-particle Raman spectroscopy will be the focus below.

4.1 Multiphase formation of secondary inorganic aerosols (SIAs)

Particulate sulfate and nitrate are two major secondary inorganic aerosols (SIAs). They have dominant Raman peaks at ∼980 and ∼1046 cm−1, respectively. Probing multiphase formation of sulfate by single-particle Raman spectroscopy was first employed by Davis and co-workers for absorption of SO2 by alkali-metal hydroxides particles (Aardahl and Davis, 1996). In atmospheric applications, particulate sulfate formation has been a debating topic since the currently proposed pathways, including O3, OH, NO2, H2O2,, and transition metal ions (TMI) in cloud water, cannot entirely account for the high concentration of sulfate observed in haze events such as those in the North China Plain (NCP) (Cheng et al., 2016). Using single-particle micro-Raman spectroscopy, Chan and his group reported that oxidants, including NO2, N(III), OH radicals, etc., generated from particulate nitrate photolysis could effectively oxidize SO2 to sulfate (Gen et al., 2019c, b; R. Zhang et al., 2020; H. Zheng et al., 2020). Clear increase in the sulfate peak signal was identified in Raman spectra of UV irradiated nitrate particle (Fig. 4). Later, they also reported sulfate formation by multiphase oxidation of SO2 during FeCl3 photolysis (Gen et al., 2020). Recently, sulfate formation was used to indicate the synergistic effect of the coexistence of iron–organic complexes and nitrate under irradiation as a source of N(III), based on the reaction between SO2 and N(III) (Gen et al., 2021). Angle et al. (2021) reported an enhanced sulfate formation in TMI-containing droplets compared to that in TMI bulk solutions. This enhancement is greater than what can be explained by the higher TMI/bisulfite concentrations in aerosol than in bulk. It suggests that surface effects and potentially aerosol pH gradients play important roles in the S(IV) oxidation process in aqueous aerosols (Angle et al., 2021).

https://acp.copernicus.org/articles/22/3017/2022/acp-22-3017-2022-f04

Figure 4Sulfate formation during the photolysis of AN particles in the presence of SO2 at 80 % RH (Gen et al., 2019c).

The formation of nitrate has also been investigated. Zangmeister and Pemberton (2001) performed kinetic analysis on the reactions between deposited NaCl particles and gaseous HNO3 based on the increase in the nitrate peak (Zangmeister and Pemberton, 2001). Tang et al. (2014) coupled optical levitation with Raman spectroscopy to investigate N2O5 uptake on SiO2 particle as a function of RH and found that particulate nitrate formation increased as RH increased. They conclude that the water content affects the partitioning of HNO3 between the gas phase and condensed phases (i.e., adsorbed phase and aqueous phase). More surface-adsorbed water layers block the reactive sites for N2O5 uptake but promote HNO3 dissolution (Tang et al., 2014). Scolaro et al. (2009) studied the three-dimensional evolution of the NaCl(100) surface during its reaction with NO2 as a function of RH, using confocal Raman imaging combined with non-contact atomic force microscopy (AFM) (Scolaro et al., 2009). At 0 % RH, a NaNO3 monolayer capping the NaCl(100) surface formed. NaNO3 tetrahedral crystals (<0.5µm) formed at 45 % RH, and supermicron NaNO3 rhombohedral plates were obtained under the H2O multilayer regime (45 % < RH <75 %). At RH >80 %, both crystalline and aqueous NO3- were found. Reactions were accelerated in the presence of water vapor due to the formation of reactive HNO3 by NO2 hydrolysis. Ault et al. (2014) reported that individual nascent sea spray aerosol particles showed different reactivity towards HNO3 and N2O5, likely due to compositional heterogeneity. After the same exposure of gaseous reactants, some particles showed intense v(NO3-) peak, whereas v(C−H) is still the dominant mode in some other particles (Ault et al., 2014).

There are also investigations on the simultaneous formation of particulate sulfate and nitrate. Zhao et al. (2018) reported a multi-step reaction mechanism of oxidation of SO2 by NO2 on deposited CaCO3 particles (Zhao et al., 2018). Further, Yu et al. (2018) reported that the uptake coefficient of SO2 on CaCO3 particles in the presence of O2/NO2 mixture was much higher than that without O2 (Yu et al., 2018). The synergy of NO2 and O2, which involved mechanisms such as chain reactions, resulted in much faster sulfate formation than the sum of the reaction rates with NO2 and with O2 alone. These reports show the usefulness of single-particle Raman spectroscopy in studying the multiphase formation of particulate sulfate and nitrate. It is worth mentioning that degradation of organo-sulfate has been proposed to produce particulate inorganic sulfate recently (R. Xu et al., 2020), and organo-sulfate functional groups are also Raman-active (Bondy et al., 2018). Raman spectroscopy may find applications in the study of organo-sulfates.

4.2 Multiphase formation of SOA

Most of the organic compounds are Raman-active, though some of them may not have strong signals. Some generate fluorescence in general orders of magnitude stronger than Raman emissions, masking useful Raman features of particles. The characteristic peaks of a single organic compound are generally more than that of an inorganic one due to its complex molecular vibration modes, and the reaction products may further complicate spectra analysis. Therefore, investigation on the multiphase formation of SOA by Raman spectroscopy is limited. However, though identifying the molecular nature of the products is difficult, single-particle Raman spectroscopy can provide useful information during secondary organic aerosol (SOA) formation. For example, Lee et al. (2008b) observed a gradually elevating baseline in Raman spectra during acid-catalyzed octanol uptake by levitated sulfuric acid particles at 10 % RH but not at 50 % RH (Lee et al., 2008b). Though the speciation of products could not be resolved, the increasing fluorescence is evident, attributable to the formed SOA in the particles. Using an EDB, Chan and Chan (2011) examined the dependence of nonanal on the presence of hydrophilic and hydrophobic organics in acidic mixed organic–sulfuric-acid particles. The presence of hydrophobic organic materials (oleic acid and its reaction products with sulfuric acid) enhanced SOA formation by reactive uptake of nonanal, likely through an enhanced dissolution of nonanal in the particles (Chan and Chan, 2011). In contrast, levoglucosan, a hydrophilic organic, did not increase the uptake coefficient of nonanal. It is suggested that acid-catalyzed reactive uptake should be examined with the explicit consideration of the role of particle-phase organics that are either initially present or accumulated as a reaction product. Using micro-Raman, Olson et al. (2019) investigated the uptake of isoprene epoxydiol (IEPOX) by α-pinene SOA/toluene SOA-coated AS particles (Olson et al., 2019). Before the uptake, both coated AS particles show core–shell morphology. v(N−H) and v(SO42-) were found at ∼3200 and ∼976 cm−1 in the particle core, while strong v(C−H) at 2800–3000 cm−1 and other moderate/weak stretches of C−H were found in the shell region. After the uptake, v(C−H) and v(RO−SO3) were found in the particle core, indicating SOA formation, such as organo-sulfate. No organo-sulfate was detected in shell regions of both types of particles, although decreases in v(C−H) peak were apparent. Generally, Raman analysis is useful for kinetic analysis of reactions (e.g., measuring uptake coefficients), but it is challenging to reveal complicated mechanisms due to the limited molecular identification. For better examining the reaction mechanism, deposited particles can be extracted for offline analysis using mass spectrometry (MS) (Li et al., 2008; Chan et al., 2013).

4.3 Multiphase oxidation of aerosol particles

In addition to reactive uptake of SOA precursors, single-particle Raman spectroscopy has also been used to explore the uptake of oxidants by organic aerosol particles. So far, the reported studies are limited to ozonolysis. Raman spectroscopy is well suited in ozonolysis studies because the C=C bonds and the peroxide groups are Raman-active, and ozonolysis does not generate strongly fluorescent products. Using single-particle Raman spectroscopy, Lee and Chan (2007a) performed in situ observations of the particle mass, hygroscopicity, morphology of the oleic acid (Lee and Chan, 2007a), linolenic acid, and linoleic acid particles (Lee and Chan, 2007b) during ozonolysis. They found that low ozone concentration ( 200–250 ppb) with a longer exposure period (20 h) favors autoxidation to form C=C-C=C groups, but an extremely high ozone concentration (∼10 ppm) at shorter exposure time (2 h) tends to form carboxylic acids (C=O), secondary ozonide (O−O), hydroxyalkyl hydroperoxide (O−H), etc. (Enami and Colussi, 2017; Qiu et al., 2020). Chu et al. (2019) further examined the interchangeability between ozone concentration and exposure time by studying ozonolysis of linoleic acid particles in a broader range of experimental conditions. They found the interchangeability holds at ozone exposure ≤500 ppb h and [O3] ≤100 ppb for the formation of autoxidation products containing conjugated diene structures but does not hold for the decay of parent linoleic acid or at higher [O3] (Chu et al., 2019). These results indicate that extrapolating experimental results of the ozonolysis under high-[O3] conditions to ambient levels should be carried out with caution. Single-particle Raman spectroscopy also enables us to infer the volatilization of some ozonolysis products. For example, Lee and Chan (2007b) found that the mass of oleic acid particles was observed to decrease with time while that of linoleic acid and linolenic acid increased on the contrary, which could be potentially explained by the different volatility of the ozonolysis products (Lee and Chan, 2007b). King et al. (2004) reported an optical tweezer study of ozonolysis of oleic acid and synthetic seawater droplets. They found clear Raman signatures indicating nonanoic acid and nonanal production, followed by their gradual disappearance, which is also likely due to the volatilization (King et al., 2004). Furthermore, Dennis-Smither et al. (2012) used optical tweezers to study the oxidation of oleic acid droplets containing an inorganic seed with a time resolution of 1 s to resolve the reactive loss of ozone and the evaporative loss of products. The oleic acid ozonolysis was completed in ∼3000 s, but the decrease in droplet volume still lasts for an additional ∼5000 s due to the slow volatilization of the products (Dennis-Smither et al., 2012).

Chan and Chan (2012) studied the roles of the phase state and water content in the ozonolysis of maleic acid (MA) and AS mixed particles. Aqueous MA was found to be more reactive towards ozone than crystalline MA. Interestingly, they also found that higher water content favors more efficient ozonolysis, although the concentration of MA is accordingly lower (Chan and Chan, 2012). Furthermore, ozonolysis of optically trapped bioaerosol particles has also been reported. In general, lipids and proteins show distinct v(C−H) peaks at 2855 and 2928 cm−1, respectively (Kline and Treado, 1997; Rygula et al., 2013; Czamara et al., 2015). The ratio of these peaks can be thus used for inferring the different susceptibilities of lipids and proteins during ozonolysis oxidation (Gong et al., 2019). The products derived from oxidations such as carbonyls (C=O; ∼1700 cm−1) (Lee and Chan, 2007b) and oligomers of cysteine (C−S; ∼662 cm−1) (Movasaghi et al., 2007; Kampf et al., 2015) are also detected.

There are also studies exploring other organic surrogates of atmospheric aerosol with more complicated structures. For example, King et al. (2008) measured the uptake coefficients of ozone on fumarate and benzoate droplets (as a proxy of HULIS-containing aerosol) and α-pinene droplets (a proxy of biogenic organic aerosol) (King et al., 2008). Different reaction products such as carbonate were identified in Raman spectra, though the chemical characterization is not comprehensive due to their volatility and the detection limits. The reaction of α-pinene in the droplet phase was more than 1 order faster than in bulk aqueous solutions, likely due to more effective diffusion of ozone in the gas phase and more efficient mass accommodation at the air–droplet interface (King et al., 2008). Milsom et al. (2021) reported the ozonolysis of fatty-acid–soap mixed particles, using oleic acid and sodium oleate as models. In these particles, the strong interactions between the soap carboxylate and the carboxylic acid form crystalline structures (Milsom et al., 2021). Upon ozonolysis, the decay of C=C (∼1600 cm−1) was faster in liquid oleic acid droplets than crystalline oleic-acid–soap particles, although the crystalline structure was eventually broken by ozonolysis. Uraoka et al. (2017) studied the multiphase reactions of optically trapped soot particles with ozone and OH radicals. C=O vibrations were observed under both ozone and OH exposure. The graphitic domain was suggested to undergo OH oxidation based on the increase in the ratio of the disorder (D) to the graphite (G) domain from Raman spectra (Uraoka et al., 2017).

4.4 Amine and ammonia reactions

Ammonia and amines are the most abundant alkaline gases in the atmosphere. They play a significant role in new particle formation and buffering aerosol pH by neutralization of acidic particles (Kirkby et al., 2011; Almeida et al., 2013; Zhang et al., 2015; Kerminen et al., 2018; G. Zheng et al., 2020; Tian et al., 2022). There are three common types of reactions involving ammonia and amines: (1) neutralization reaction between acidic particles and ammonia or amines; (2) displacement of ammonia by amines from ammonium salt particles and vice versa from aminium salt particles; (3) reactions between ammonia or amines and dissolved dicarbonyls or between gaseous dicarbonyls and ammonium or aminium salt particles – both would result in the formation of colored compounds (i.e., brown carbon; BrC).

Based on the strong vibration signal of the C−H bond (∼2900 cm−1, sharp peak) from amine or aminium salts and the N−H bond ( 2800–3300 cm−1, broad peak), the uptake of amine and ammonia can be easily studied using single-particle Raman spectroscopy. Sauerwein and Chan (2017) explored the role of phase state in simultaneous uptake of ammonia and dimethylamine (DMA) by acidic particles (e.g., sulfuric acid and oxalic acid). Anhydrous acidic particles were inert and took up DMA and ammonia presumably by adsorption and absorption only. The uptake rates of DMA and ammonia by aqueous acidic droplets were found to be comparable initially, but once the droplets were neutralized, the stronger base DMA displaced some of the particulate ammonium. On the other hand, if crystallization took place during the uptake, DMA uptake was inhibited, but continuous ammonia uptake gradually displaced the particle DMA ions.

Chan and Chan (2013) reported that the exchange reactions of ammonia/amine vapors in aqueous particles were reversible, and the exchange rates of aqueous particles were, in general, higher than those of their corresponding solid counterparts. Compared with crystalline solids (e.g., methylammonium sulfate), amorphous solid (e.g., diethylammonium sulfate) was found with a higher exchange rate, likely due to the less compact molecular structure (Chan and Chan, 2013). Chu and Chan (2017a, b) further examined the effect of a hydrophilic viscous organic surrogate and a hydrophobic organic coating on DMA uptake by AS. Both the viscous materials and the fresh and aged organic coating retarded DMA uptake by mass-transfer limitation (Chu and Chan, 2017a, b). The uptake of DMA by crystallized AS particles at 10 %–30 % RH resulted in the deliquescence of the particles, likely due to the presence of surface-adsorbed water (SAW) that promoted the dissolution of DMA. Once dimethylaminium sulfate is formed, it absorbs more water since it is more hygroscopic than AS and further promoted DMA uptake (Chu and Chan, 2017b). As crystalline solids are generally considered inert towards reactions, this finding indicates that SAW on crystals can serve as a medium to facilitate gas uptake.

BrC has attracted increasing attention due to its atmospheric abundance and capacity in regulating radiative balance (Laskin et al., 2015). The reactions between dicarbonyls and ammonium/aminium-containing salt particles can form BrC. Gen et al. (2018) investigated the multiphase uptake of glyoxal by ammonium-salt-containing particles using micro-Raman spectroscopy. They found a gradual elevation of the baseline, which was attributed to the formation of a fluorescent BrC (i.e., 2,2-biimidazole, BI), based on offline analysis by UV–Vis spectroscopy and fluorescence spectroscopy (Gen et al., 2018). The reduction in ALW at low RH increases the glyoxal uptake rate via the enhanced salting-in effect and the BI formation rate by facilitating dehydration reactions. Mabato et al. (2019) examined glyoxal uptake by methylaminium-salt-containing particles. Although the salting-in effect was also found in methylaminium-salt-containing particles, enhanced BI formation was not observed, likely due to the higher hygroscopicity of methylaminium salt (i.e., higher ALW content) than ammonium salt (Mabato et al., 2019).

4.5 Photochemistry of aerosol particles

A particular type of aerosol particle reaction that deserves special attention is photochemical reactions, which can be initiated by irradiation of the particles. Nitrate can be photolyzed under atmospheric irradiation (λ>290 nm). Nitrate photolysis proceeds via three channels: one produces NO2 and OH radicals, another produces NO2- and O(3P), and the last generates ONOO (Scharko et al., 2014; Benedict et al., 2017). The third channel's quantum yield is considered negligible compared with the former two since ONOO is unstable (Mabato et al., 2022). Particulate nitrate photolysis in the atmospheric has been reviewed by a recent paper (Gen et al., 2022). It has been reported that NO2- and ONOO peaks increased, but NO3- peaks decreased in the Raman spectra of acoustically levitated nitrate particles irradiated by UV (Tobon et al., 2017). NO2 does not have a large absorption cross-section, but it may be hydrolyzed into NO2- (Tobon et al., 2017; Seng et al., 2018; Gómez Castaño et al., 2019). Most nitrate photolysis products are oxidants, so their ability to initiate oxidation reactions has also been explored (Gen et al., 2019b, c; R. Zhang et al., 2020). The production of sulfate via nitrate photolysis was discussed earlier. Recently, R. Zhang et al. (2021) reported a prominent formate production by glyoxal oxidation during particulate nitrate photolysis, instead of the more commonly found oxalic acids in the oxidation of glyoxal in bulk solutions (R. Zhang et al., 2021; Tan et al., 2009; Zhang et al., 2019). Furthermore, Liang et al. (2021) studied nitrate photolysis in particles containing sucrose, which was used as a surrogate for atmospheric viscous organics. They found that the viscosity of the particle did not reduce the nitrate photolysis rate, but it limited the diffusion of gaseous products (e.g., NOx, NOy) from nitrate photolysis. At a high sucrose fraction and 30 % RH, the production of these gaseous products and the particles' viscosity transformed the droplets into “hollow and enlarged” semi-solid particles. Very recently, Zhang et al (2022) reported an enhanced decay of glyoxal by a factor of 12 in NH4NO3/glyoxal premixed particles, compared to that under dark condition, due to nitrate photolysis and BrC-induced (e.g., imidazole-2-carboxaldehyde) photosensitization. Using a Raman microscope, a new organic phase was observed in irradiated NH4NO3/glyoxal droplets with no noticeable degradation under prolonged photooxidation, which may contribute to atmospheric SOA formation.

Size dependence of nitrate photochemistry has been recently reported, based on single-particle Raman spectroscopy. Tobon et al. (2017) studied the photolysis of acoustically levitated nitrate particles (40–80 µm) at 254 nm UV radiation. No change in Raman spectra was observed for 2 h. In contrast, smaller particles (5–8 µm) trapped optically yielded various Raman peaks of nitrate photolysis products (Tobon et al., 2017; Gómez Castaño et al., 2019). The slow photolysis in the larger nitrate particles was attributed to the self-inhibited surface process. Additionally, an uneven distribution of NO2- inside the smaller particle was also observed through Raman mapping (Gómez Castaño et al., 2019). Organics in the aerosol particle may also decompose under light. For example, Parmentier et al. (2021) reported photodegradation of optically trapped oleic acid droplets under 532 and 660 nm irradiation, likely initiated by photosensitization. However, they cautioned that the degradation loss of optically trapped particles might be due to artifacts (Parmentier et al., 2021). The photo-decay of light-absorbing particulate matter is also of great interest in understanding its fate in the atmosphere. However, there are very limited studies of atmospheric photochemical reactions using Raman spectroscopy, partly because of the need for complementary chemical speciation for detailed mechanistic studies.

5 Enhanced Raman spectroscopy

Though Raman spectroscopy has been used to study physical and chemical processes of atmospheric particles, most of the studies used large particles (dozens of microns) and focused on lab-generated particles with a few representative components. That is primarily because of the intrinsic diffraction limitation of Raman measurements that the laser beam cannot be effectively focused to a spot smaller than its wavelength and thus limits the detection of particles to larger than 1 micron or so. Fluorescence can also be a complication in some chemical systems.

Various methods have been developed to improve the Raman signal-to-noise ratios and the spatial resolution in other research fields such as material science and biology. Surface-enhanced Raman spectroscopy (SERS) and tip-enhanced Raman spectroscopy (TERS) have been recently employed in atmospheric research. SERS and TERS enhance Raman emissions by the localized surface plasmon resonances using noble metal nanoparticles (NPs) to provide hot spots near the contacting sites between the analyte and NPs (Ault and Axson, 2017). According to the SERS electromagnetic (EM) enhancement theory, the relationship between the SERS intensity (I) and the local EM strength (E) follows I|E|4. The relationship between E and the distance between NPs and analytes (D) is described as E (1/D) (Zhou et al., 2015). Hence, maximizing E and minimizing D without inducing significant perturbation to the sample is the primary goal. In addition to this physical enhancement based on the electromagnetic field, Raman signals can also be enhanced chemically. Specifically, molecular/ionic species can attach to the surface of NPs, distorting the molecular structure and increasing the absorption cross-section. Consequently, the Raman signal of an adsorbed species can be enhanced, potentially accompanied by a peak shift (Craig et al., 2015; Gen and Chan, 2017).

SERS enables the measurements of single particles smaller than 1 micron. Craig et al. (2015) found that the signals from individual submicron (down to 0.6 µm) particles could be effectively detected with intensity enhancement (Craig et al., 2015). Furthermore, Tirella et al. (2018) extended the SERS detection to the accumulation mode (800–150 nm) particles (Tirella et al., 2018). Sun et al. (2019a, b) reported a size-resolved (covering both coarse mode and accumulation mode) SERS characterization study of atmospheric particles sampled during haze events (Sun et al., 2019a, b). More recently, Kunihisa et al. (2020) reported sensitive SERS measurement of Aitken mode particles (<100 nm) by combining a condensational growth tube sampler (CGT) and a SERS substrate for directly sampling (Kunihisa et al., 2020). The wide analytical range of particle size enables SERS to be a potentially powerful tool in studying ambient particulate matters (Steer et al., 2016; Vejpongsa et al., 2017; Chen et al., 2021).

Some species including components of microorganisms (Tahir et al., 2020), microplastics (G. Xu et al., 2020), crystalline silica (Zheng et al., 2018), the fine structure of organics (Craig et al., 2015; Fu et al., 2017; Gen et al., 2018), and even some Raman-active inorganic salts at very low concentration (Saniel et al., 2019) are invisible in normal Raman due to their weak Raman activities. However, they could be detected with a SERS substrate. The sensitive detection by SERS can provide valuable insight into particle transformations and emission sources (Vejpongsa et al., 2017; Ghosal and Wall, 2019; Lee et al., 2019). However, the enhancement factor of SERS is not constant. It strongly depends on the distribution and quantity of noble metal NPs and the hot spots over the substrate, making quantitative analysis difficult. Many attempts have been made to explore preferable and tunable substrate for generalizable atmospheric particle detection (G. Xu et al., 2020; Cheng et al., 2021), but still more progress is needed in the future.

The most common SERS application uses particles deposited on SERS substrates, relying on the hot spot located beneath the analyte particles. Recently, some studies create innovative interactions between particulate analytes and SERS NPs to enhance SERS detections. Wei et al. (2018) used 4-mercaptobenzoic acid-functionalized AuNPs as pH nanoprobes and internal SERS substrate and found the existence of a stable pH gradient inside aqueous particles (Wei et al., 2018). Hence, the assumption of homogeneous mixing might not always be correct, and pH predictions by thermodynamic model might underestimate the acidity of interfacial layers of particles, which is crucial for multiphase uptake or surface reactions. As a further investigation of the SERS pH nanoprobe, Q. Huang et al. (2021) reported that the pH distribution inside aerosol particles is affected by the internal distribution of ions, which may depend on the ionic speciation. While sodium tends to reside in the bulk of the particle, leading to a high centroid pH, pH distributes more evenly in ammonium salt droplets because ammonium has a higher surface propensity than sodium (Q. Huang et al., 2021).

Gen and Chan (2017) developed an electrospray system (ES-SERS) to deposit SERS NPs onto the surface of the analyte particle and found that this technique can selectively enhance the peak intensity of the species located at surface layers such as surface-adsorbed water (Gen and Chan, 2017) and organic coatings (Gen et al., 2019a). In a typical micro-Raman setup, the objective is above the analyte particle. When the analyte particle is deposited on the SERS substrate, the SERS hot spots are located beneath the particle. In other words, upon laser irradiation from the top, the photons generated by excitation need to pass through the particle with a refractive index greater than air, which would scatter or absorb light and thus reduce the signals received by the Raman microscope. In contrast, ES-SERS hot spots are created on the surface of the particle using electrospray. This configuration reduces the loss of photons and affords greater enhancement in the Raman intensity (Fig. 5). Besides, as the SERS effect is much more prominent near the hot spots, the location of the hot spot determines what part of the particle will be probed. Therefore, while typical SERS substrate collects enhanced Raman signals from the substrate–particle interface, the ES-SERS can provide information from the gas–particle interface, where many atmospheric multiphase processes occur. Sivaprakasam et al. (2017) and Sivaprakasam and Hart (2021) reported real-time SERS measurements of electrostatically trapped particles containing analyte molecules and NPs as internally mixed liquid particles or coating on solid particles (Sivaprakasam et al., 2017; Sivaprakasam and Hart, 2021). The interaction between NPs and analyte increased due to more contact areas than between an aerosol particle and a substrate.

https://acp.copernicus.org/articles/22/3017/2022/acp-22-3017-2022-f05

Figure 5Schematic illustration of (a) a conventional SERS substrate approach and (b) the ES-SERS approach (Gen and Chan, 2017).

Similarly, TERS can produce enhanced Raman signals even from particles in the nucleation mode. TERS is a combination of an atomic force microscope (AFM) and a Raman spectrometer. In general, the AFM determines the topography of a single deposited particle by detecting the interaction force between the AFM tip and the surface of the analytes. In a typical TERS setup, the AFM tip is coated with noble metal particles. An enhanced Raman signal is generated when the tip is interacting with analytes under laser excitation (Rodriguez et al., 2015). The lack of chemical information of AFM is complemented by SERS. Thus, TERS enables simultaneous characterization of particulate topography and surface species of submicron particles at a high spatial resolution (Ofner et al., 2016). TERS also has the potential for quantitative analysis since the quantity and configuration of hot spots on the tip are constant.

6 Bioaerosols

Bioaerosols have attracted increasing attention worldwide due to the COVID-19 epidemic. Studies using normal Raman/SERS for offline detection of biological samples (Félix-Rivera and Hernández-Rivera, 2012; Mosier-Boss, 2017) and real-time sensing of bioaerosol (Huffman et al., 2020) have been reviewed in detail elsewhere. Bioaerosols have various Raman-active components such as phosphate lipid (δ (=C-H), ∼1268 cm−1; v(C−H), ∼2855cm−1), protein (amides bands, ∼1260, ∼1600, ∼1660 cm−1; C−C backbone stretching in β-sheet proteins, ∼983 cm−1; v(C−H), ∼2928 cm−1), and nucleic acids (e.g., adenine, ∼735 cm−1) (Socrates, 2004; Rygula et al., 2013; Talari et al., 2015). However, Raman signals from bioaerosol particles are generally weak. To amplify the signals, bioaerosol particles are trapped or deposited onto a substrate for longer integration time (Laucks et al., 2000; Sengupta et al., 2005; Tripathi et al., 2009; C. Wang et al., 2015; Redding et al., 2015b; Ai et al., 2020). Using a higher-energy laser can also enhance Raman intensity, but it may cause damage to bioaerosol (e.g., fragmentation) (Gong et al., 2017). On this basis, SERS is more suitable than normal Raman spectroscopy. SERS can also quench the fluorescence generated by biomolecules such as tryptophan and tyrosine (Gong et al., 2017).

In general, there are two strategies of single-particle SERS of bioaerosols: (1) directly sampling bioaerosols on a SERS substrate; (2) moving mixed colloids of SERS NPs and bioaerosols onto a glass substrate, followed by drying. While the former is more convenient without complex pretreatments (Tahir et al., 2020), the latter enables flexible modification of NP properties. For example, the functionalized surface of NPs with tag molecules (e.g., antibody), so-called label-based SERS (Liu et al., 2010), was used for detecting specific biomaterials with high reproducibility. Label-free SERS refers to that without tag molecules, such as Au@Ag (i.e., Au core with Ag shell). In general, by simply mixing, NPs distribute on biomaterials without specific interactions, and the SERS reproducibility is limited. However, by coating AgNPs on the cell wall of bacteria (H. Zhou et al., 2014, 2015), SERS enhancement was ∼30-folds reproducibly higher than simply mixed colloid–bacterial suspension. Furthermore, the discrimination of live and dead bacteria was possible. NPs can be directly formed inside some specific bacteria via bio-reduction for probing the intercellular structure (Jarvis et al., 2008). Overall, SERS can be an innovative tool in bioaerosol characterization, but the antibacterial effect of NPs and heat effect due to excitation laser should be considered (Mosier-Boss, 2017). More examples of bioaerosol detection can be found in a recent review (Liu et al., 2017).

7 Future directions

This review paper has shown examples of single-particle Raman spectroscopy in studying atmospheric processes. Overall, the water content, phase state, morphology, and chemical composition of single particles during physical and chemical processes at controlled RH can be monitored in situ. Hygroscopicity and phase behaviors covering a wide range of RH after these processes can also be comprehensively assessed by performing evaporation–humidification cycle measurements (Chan et al., 2006; Chan and Chan, 2007; Liu et al., 2008; Chen et al., 2020). Although fluorescence may exist in some particles, it could be potentially reduced or even eliminated by (1) using longer excitation wavelengths (e.g., 785 and 1064 nm), (2) employing SERS/TERS, and (3) photo-bleaching of fluorescent substances under UV–Vis illumination (Gong et al., 2017). There are many other innovative studies built on trapping, manipulating, and observing multi-particles via Raman (Mitchem and Reid, 2008; Davies, 2019), such as measuring the viscosity and diffusion coefficient (Power et al., 2013; Nakajima et al., 2021), probing reaction (Aardahl et al., 1998; Rkiouak et al., 2014), and phase transition (Richards et al., 2020). Based on these functions and research progress, we would like to provide the following suggestions on future directions.

  • Combining other techniques with single-particle Raman spectroscopy. Raman spectroscopy is non-destructive, so incorporating other spectroscopic techniques for characterizing the same particle is possible. Vibrational sum frequency generation spectroscopy (SFG), Fourier transform infrared spectroscopy (FTIR), and fluorescence spectroscopy, which are also non-destructive, could be complementary to Raman in probing the chemical composition of single particles. Recently, novel combination of EDB and mass spectrometry was reported, which can directly introduce the trapped particle for mass spectrometry analysis (Jacobs et al., 2017; Birdsall et al., 2018; Willis et al., 2020). Adoption of this technique with Raman to form an EDB–Raman system with subsequent MS analysis is relatively straightforward. For optical properties, UV–Vis spectroscopy could be a promising choice (Jones et al., 2021). While general laser-based MDR can easily bleach light-absorbing molecules, a recent study reported that MDR modes under broadband excitation can measure refractive index (RI) of light-sensitive samples (Price et al., 2020). Such MDR measurements can complement in situ Raman spectroscopy for chemical characterization. Additionally, SERS and TERS are emerging useful approaches, but current SERS and TERS methods for atmospheric research mainly use bare NPs. The direct contact of NPs to analyte molecules can potentially induce chemical enhancement, which could complicate the identification of the phase transition and functional groups (Craig et al., 2015; Gen and Chan, 2017). To remove the chemical enhancement, future studies on chemically inert NPs such as shell-isolated nanoparticle-enhanced Raman spectroscopy (SHINERS) are suggested (Li et al., 2010; Anema et al., 2011).

  • Multiphase reaction studies based on single-particle Raman spectroscopy. Single-particle Raman spectroscopy enables investigations of various atmospheric reactions, including those in surface-adsorbed water for solids, mixed-phase particles (solid, aqueous, organic), supersaturated droplets, atmospheric aging of bioaerosols, and ultrafast reactions. For solid particles (e.g., crystalline, mineral dust), multiphase reactions can be mediated by surface-adsorbed water layers and may result in phase transition, turning the particle into liquid for further reactions (Kuwata and Martin, 2012; Chu and Chan, 2017b; Zhao et al., 2018; Yu et al., 2018; Gen et al., 2019a). Probing heterogenous reactions on the particle surface is possible via ES-SERS, TERS, and normal Raman imaging. As particle constituents can be unevenly distributed (e.g., in LLPS) within a single particle, chemistry may not be the same between the bulk and the surface layers (Wei et al., 2018; Olson et al., 2019; Qiu et al., 2019; Q. Huang et al., 2021; Lam et al., 2021). The studies of the atmospheric processing of pre-existing particles to form secondary aerosols can be further extended to the aging of bioaerosols (Gong et al., 2019). Using pulse laser for excitation, time-resolved resonance Raman spectroscopy (TR3) can be a promising tool in probing short-lived reactive intermediates (e.g., triplet state molecules). In particular, it helps deepen our understanding in ultrafast reactions or initiation steps of typical reactions (Sahoo et al., 2011; Collins et al., 2018).

  • Particle size and temperature effects. Many publications report single-particle Raman spectroscopy studies under different environmental conditions, including RH and gas concentration. However, how experimental conditions such as temperature and particle size affect kinetics and products in multiphase reactions remains ambiguous. For example, various pathways and kinetic parameters have been proposed to explain particulate sulfate formation in winter haze events in northern China (Chan and Yao, 2008; Su et al., 2020; Liu et al., 2021). However, most studies are based on experimental results at room temperature or 298 K. Further exploration with respect to the effect of low temperature on the properties of the particles and multiphase sulfate chemistry is still warranted. Employing a temperature-controlled cold-plate flow-cell–Raman system for deposited single particles (Wheeler et al., 2015; Mael et al., 2019; Roy et al., 2020), investigations of temperature-dependent reaction kinetics can be easily achieved. Temperature control in a small levitation chamber is also more convenient than in a flow tube or smog chamber. To date, almost all single-particle Raman studies involve supermicron particles. While equilibrium measurements are not sensitive to size (assuming the Kelvin effect is considered), kinetic analysis is often size-dependent. Hence, uptake coefficients for multiphase reactions are usually reported and are restricted to experimental conditions that gas- and liquid-phase transport are not the rate-limiting step. The size detection limit of single-particle Raman spectroscopy can be extended to sub-10 µm with high sensitivity using high-energy excitation laser and tighter optical focusing. The effect of temperature and particle size on multiphase chemistry should be further investigated using long integration time, novel optical configuration (e.g., confocal micro-Raman), and SERS/TERS. Although it is challenging to study single submicron particles by Raman spectroscopy regularly, Raman characterization of a collection of single submicron particles is feasible.

Appendix A

Table A1Major Raman peaks of atmospherically relevant species.

Download Print Version | Download XLSX

Data availability

All datasets are provided in Appendix A.

Author contributions

ZL and CKC conceptualized the work. ZL, YC, MG, and CKC prepared the original draft and contributed to the review and editing.

Competing interests

The contact author has declared that neither they nor their co-authors have any competing interests.

Disclaimer

Publisher’s note: Copernicus Publications remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.

Acknowledgements

We gratefully acknowledge the support from the National Natural Science Foundation of China (grant nos. 41905122, 42075100, and 41875142), the Hong Kong Research Grants Council (grant no. 11302318), the Japan Science and Technology Agency (JST) Fusion Oriented Research for disruptive Science and Technology program (grant no. 20352853), and the Japan Society for the Promotion of Science (JSPS) Grants-in-Aid for Early-Career Scientists (grant no. 21K17876).

Financial support

This research has been supported by the National Natural Science Foundation of China (grant nos. 41905122, 42075100, and 41875142); the Research Grants Council, University Grants Committee (grant no. 11302318); the Japan Science and Technology Agency (grant no. 20352853); and the Japan Society for the Promotion of Science (grant no. 21K17876).

Review statement

This paper was edited by Jason Surratt and reviewed by two anonymous referees.

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The properties and fate of individual airborne particles can be significantly different, leading to distinct environmental impacts (e.g., climate and human health). While many instruments only analyze an ensemble of these particles, single-particle Raman spectroscopy enables unambiguous characterization of individual particles. This paper comprehensively reviews the applications of such a technique in studying atmospheric particles, especially for their physicochemical processing.
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