Articles | Volume 23, issue 15
https://doi.org/10.5194/acp-23-8979-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-23-8979-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
11 Aug 2023
Research article |
| 11 Aug 2023
| 11 Aug 2023
Direct observation for relative-humidity-dependent mixing states of submicron particles containing organic surfactants and inorganic salts
Chun Xiong
Zhejiang Provincial Key Laboratory of Organic Pollution Process and Control, MOE Key Laboratory of Environment Remediation and Ecological Health, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China
Binyu Kuang
Zhejiang Provincial Key Laboratory of Organic Pollution Process and Control, MOE Key Laboratory of Environment Remediation and Ecological Health, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China
Fei Zhang
Zhejiang Provincial Key Laboratory of Organic Pollution Process and Control, MOE Key Laboratory of Environment Remediation and Ecological Health, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China
Xiangyu Pei
Zhejiang Provincial Key Laboratory of Organic Pollution Process and Control, MOE Key Laboratory of Environment Remediation and Ecological Health, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China
Zhengning Xu
Zhejiang Provincial Key Laboratory of Organic Pollution Process and Control, MOE Key Laboratory of Environment Remediation and Ecological Health, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China
Zhibin Wang
CORRESPONDING AUTHOR
Zhejiang Provincial Key Laboratory of Organic Pollution Process and Control, MOE Key Laboratory of Environment Remediation and Ecological Health, College of Environmental and Resource Sciences, Zhejiang University, Hangzhou 310058, China
ZJU–Hangzhou Global Scientific and Technological Innovation Center, Zhejiang University, Hangzhou 311215, China
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Yuxuan Zhang, Qiang Zhang, Yafang Cheng, Hang Su, Simonas Kecorius, Zhibin Wang, Zhijun Wu, Min Hu, Tong Zhu, Alfred Wiedensohler, and Kebin He
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Z. J. Wu, L. Poulain, W. Birmili, J. Größ, N. Niedermeier, Z. B. Wang, H. Herrmann, and A. Wiedensohler
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Z. Wang, H. Su, X. Wang, N. Ma, A. Wiedensohler, U. Pöschl, and Y. Cheng
Atmos. Meas. Tech., 8, 2161–2172, https://doi.org/10.5194/amt-8-2161-2015, https://doi.org/10.5194/amt-8-2161-2015, 2015
Z. B. Wang, M. Hu, J. Y. Sun, Z. J. Wu, D. L. Yue, X. J. Shen, Y. M. Zhang, X. Y. Pei, Y. F. Cheng, and A. Wiedensohler
Atmos. Chem. Phys., 13, 12495–12506, https://doi.org/10.5194/acp-13-12495-2013, https://doi.org/10.5194/acp-13-12495-2013, 2013
Z. B. Wang, M. Hu, D. Mogensen, D. L. Yue, J. Zheng, R. Y. Zhang, Y. Liu, B. Yuan, X. Li, M. Shao, L. Zhou, Z. J. Wu, A. Wiedensohler, and M. Boy
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Z. B. Wang, M. Hu, Z. J. Wu, D. L. Yue, L. Y. He, X. F. Huang, X. G. Liu, and A. Wiedensohler
Atmos. Chem. Phys., 13, 10159–10170, https://doi.org/10.5194/acp-13-10159-2013, https://doi.org/10.5194/acp-13-10159-2013, 2013
Z. B. Wang, M. Hu, Z. J. Wu, D. L. Yue, J. Zheng, R. Y. Zhang, X. Y. Pei, P. Paasonen, M. Dal Maso, M. Boy, and A. Wiedensohler
Atmos. Chem. Phys. Discuss., https://doi.org/10.5194/acpd-13-3419-2013, https://doi.org/10.5194/acpd-13-3419-2013, 2013
Revised manuscript not accepted
Related subject area
Subject: Aerosols | Research Activity: Laboratory Studies | Altitude Range: Troposphere | Science Focus: Physics (physical properties and processes)
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An aerosol optical tweezer (AOT) Raman spectroscopy system is developed to capture a single aerosol droplet for phase transition monitoring and morphology studies. Rapid droplet capture is achieved and accurate droplet size and refractive index are retrieved. Results indicate that mixed inorganic/organic droplets are more inclined to form core–shell morphology when RH decreases. The phase transitions of secondary mixed organic aerosol/inorganic droplets vary with their precursors.
Baptiste Testa, Lukas Durdina, Peter A. Alpert, Fabian Mahrt, Christopher H. Dreimol, Jacinta Edebeli, Curdin Spirig, Zachary C. J. Decker, Julien Anet, and Zamin A. Kanji
Atmos. Chem. Phys., 24, 4537–4567, https://doi.org/10.5194/acp-24-4537-2024, https://doi.org/10.5194/acp-24-4537-2024, 2024
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Laboratory experiments on the ice nucleation of real commercial aviation soot particles are investigated for their cirrus cloud formation potential. Our results show that aircraft-emitted soot in the upper troposphere will be poor ice-nucleating particles. Measuring the soot particle morphology and modifying their mixing state allow us to elucidate why these particles are ineffective at forming ice, in contrast to previously used soot surrogates.
Satish Basnet, Anni Hartikainen, Aki Virkkula, Pasi Yli-Pirilä, Miika Kortelainen, Heikki Suhonen, Laura Kilpeläinen, Mika Ihalainen, Sampsa Väätäinen, Juho Louhisalmi, Markus Somero, Jarkko Tissari, Gert Jakobi, Ralf Zimmermann, Antti Kilpeläinen, and Olli Sippula
Atmos. Chem. Phys., 24, 3197–3215, https://doi.org/10.5194/acp-24-3197-2024, https://doi.org/10.5194/acp-24-3197-2024, 2024
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Brown carbon (BrC) emissions were estimated, for residential wood combustion (RWC) from various northern European appliances, utilizing an extensive seven-wavelength aethalometer dataset and thermal–optical carbon analysis. The contribution of BrC370–950 to the absorption of visible light varied between 1 % and 21 %, and was linked with fuel moisture content and combustion efficiency. This study provides important information required for assessing the climate effects of RWC emissions.
Yu-Kai Tong, Zhijun Wu, Min Hu, and Anpei Ye
Atmos. Chem. Phys., 24, 2937–2950, https://doi.org/10.5194/acp-24-2937-2024, https://doi.org/10.5194/acp-24-2937-2024, 2024
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The interplay between aerosols and moisture is one of the most crucial atmospheric processes. However, to date, literature results on the influence of phase separation on water diffusion in aerosols are divergent. This work directly unveiled the water diffusion process in single suspended phase-separated microdroplets and quantitatively analyzed the diffusion rate and extent. The results show that diffusion limitations and certain molecule clusters existed in the phase-separated aerosols.
Eugene F. Mikhailov, Sergey S. Vlasenko, and Alexei A. Kiselev
Atmos. Chem. Phys., 24, 2971–2984, https://doi.org/10.5194/acp-24-2971-2024, https://doi.org/10.5194/acp-24-2971-2024, 2024
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Surface tension and water activity are key thermodynamic parameters determining the impact of atmospheric aerosols on human health and climate. However, these parameters are not well constrained for nanoparticles composed of organic and inorganic compounds. In this study, we determined for the first time the water activity and surface tension of mixed organic/inorganic nanodroplets by applying a differential Köhler analysis (DKA) to hygroscopic growth measurements.
Joel Ponsonby, Leon King, Benjamin J. Murray, and Marc E. J. Stettler
Atmos. Chem. Phys., 24, 2045–2058, https://doi.org/10.5194/acp-24-2045-2024, https://doi.org/10.5194/acp-24-2045-2024, 2024
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Aerosol emissions from aircraft engines contribute to the formation of contrails, which have a climate impact as important as that of aviation’s CO2 emissions. For the first time, we experimentally investigate the freezing behaviour of water droplets formed on jet lubrication oil aerosol. We show that they can activate to form water droplets and discuss their potential impact on contrail formation. Our study has implications for contrails produced by future aircraft engine and fuel technologies.
Zhanyu Su, Lanxiadi Chen, Yuan Liu, Peng Zhang, Tianzeng Chen, Biwu Chu, Mingjin Tang, Qingxin Ma, and Hong He
Atmos. Chem. Phys., 24, 993–1003, https://doi.org/10.5194/acp-24-993-2024, https://doi.org/10.5194/acp-24-993-2024, 2024
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In this study, different soot particles were analyzed to better understand their behavior. It was discovered that water-soluble substances in soot facilitate water adsorption at low humidity while increasing the number of water layers at high humidity. Soot from organic fuels exhibits hygroscopicity influenced by organic carbon and microstructure. Additionally, the presence of sulfate ions due to the oxidation of SO2 enhances soot's hygroscopicity.
Eike Maximilian Esders, Sebastian Sittl, Inka Krammel, Wolfgang Babel, Georg Papastavrou, and Christoph Karl Thomas
Atmos. Chem. Phys., 23, 15835–15851, https://doi.org/10.5194/acp-23-15835-2023, https://doi.org/10.5194/acp-23-15835-2023, 2023
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Do microplastics behave differently from mineral particles when they are exposed to wind? We observed plastic and mineral particles in a wind tunnel and measured at what wind speeds the particles start to move. The results indicate that microplastics start to move at smaller wind speeds as they weigh less and are less sticky. Hence, we think that microplastics also move more easily in the environment.
Abd El Rahman El Mais, Barbara D'Anna, Luka Drinovec, Andrew T. Lambe, Zhe Peng, Jean-Eudes Petit, Olivier Favez, Selim Aït-Aïssa, and Alexandre Albinet
Atmos. Chem. Phys., 23, 15077–15096, https://doi.org/10.5194/acp-23-15077-2023, https://doi.org/10.5194/acp-23-15077-2023, 2023
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Polycyclic aromatic hydrocarbons (PAHS) and furans are key precursors of secondary organic aerosols (SOAs) related to biomass burning emissions. We evaluated and compared the formation yields, and the physical and light absorption properties, of laboratory-generated SOAs from the oxidation of such compounds for both, day- and nighttime reactivities. The results illustrate that PAHs are large SOA precursors and may contribute significantly to the biomass burning brown carbon in the atmosphere.
Haifan Zhang, Xiangyu Lin, Qinghong Zhang, Kai Bi, Chan-Pang Ng, Yangze Ren, Huiwen Xue, Li Chen, and Zhuolin Chang
Atmos. Chem. Phys., 23, 13957–13971, https://doi.org/10.5194/acp-23-13957-2023, https://doi.org/10.5194/acp-23-13957-2023, 2023
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This work is the first study to simultaneously analyze the number concentrations and species of insoluble particles in hailstones. The size distribution of insoluble particles for each species vary greatly in different hailstorms but little in shells. Two classic size distribution modes of organics and dust were fitted for the description of insoluble particles in deep convection. Combining this study with future experiments will lead to refinement of weather and climate models.
Yaru Song, Jianlong Li, Narcisse Tsona Tchinda, Kun Li, and Lin Du
EGUsphere, https://doi.org/10.5194/egusphere-2023-2011, https://doi.org/10.5194/egusphere-2023-2011, 2023
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Aromatic acids can be transferred from seawater to the atmosphere through bubble bursting. The air-sea transfer efficiency of aromatic acids was evaluated by simulating the SSA generation with a plunging jet. As a whole, the transfer capacity of aromatic acids may depend on their functional groups and on the bridging effect of cation, as well as their concentration in seawater, as these factors influence the global emission flux of aromatic acids via SSA.
Yueling Chen, Xiangyu Pei, Huichao Liu, Yikan Meng, Zhengning Xu, Fei Zhang, Chun Xiong, Thomas C. Preston, and Zhibin Wang
Atmos. Chem. Phys., 23, 10255–10265, https://doi.org/10.5194/acp-23-10255-2023, https://doi.org/10.5194/acp-23-10255-2023, 2023
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The impact of acidity on the phase transition behavior of levitated aerosol particles was examined. Our results revealed that lower acidity decreases the separation relative humidity of aerosol droplets mixed with ammonium sulfate and secondary organic aerosol proxy. Our research suggests that in real atmospheric conditions, with the high acidity found in many ambient aerosol particles, droplets encounter heightened impediments to phase separation and tend to display a homogeneous structure.
Mária Lbadaoui-Darvas, Ari Laaksonen, and Athanasios Nenes
Atmos. Chem. Phys., 23, 10057–10074, https://doi.org/10.5194/acp-23-10057-2023, https://doi.org/10.5194/acp-23-10057-2023, 2023
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Heterogeneous ice nucleation is the main ice formation mechanism in clouds. The mechanism of different freezing modes is to date unknown, which results in large model biases. Experiments do not allow for direct observation of ice nucleation at its native resolution. This work uses first principles molecular simulations to determine the mechanism of the least-understood ice nucleation mode and link it to adsorption through a novel modeling framework that unites ice and droplet formation.
Carynelisa Haspel, Cuiqi Zhang, Martin J. Wolf, Daniel J. Cziczo, and Maor Sela
Atmos. Chem. Phys., 23, 10091–10115, https://doi.org/10.5194/acp-23-10091-2023, https://doi.org/10.5194/acp-23-10091-2023, 2023
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Small particles, commonly termed aerosols, can be found throughout the atmosphere and come from both natural and anthropogenic sources. One important type of aerosol is black carbon (BC). In this study, we conducted laboratory measurements of light scattering by particles meant to mimic atmospheric BC and compared them to calculations of scattering. We find that it is likely that calculations underpredict the scattering by BC particles of certain polarizations of light in certain directions.
Azad Madhu, Myoseon Jang, and Yujin Jo
EGUsphere, https://doi.org/10.5194/egusphere-2023-1500, https://doi.org/10.5194/egusphere-2023-1500, 2023
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SOA formation from branched alkanes is simulated using the UNIPAR model which predicted SOA growth via multiphase reactions of hydrocarbons and compared with chamber data. Product distributions of branched alkanes were created by extrapolating product distributions of linear alkanes. To account for methyl branching, an autoxidation reduction factor was applied to product distributions. Branched alkanes in diesel fuel were shown to produce a higher proportion of SOA compared to linear alkanes.
Clarissa Baldo, Paola Formenti, Claudia Di Biagio, Gongda Lu, Congbo Song, Mathieu Cazaunau, Edouard Pangui, Jean-Francois Doussin, Pavla Dagsson-Waldhauserova, Olafur Arnalds, David Beddows, A. Robert MacKenzie, and Zongbo Shi
Atmos. Chem. Phys., 23, 7975–8000, https://doi.org/10.5194/acp-23-7975-2023, https://doi.org/10.5194/acp-23-7975-2023, 2023
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This paper presents new shortwave spectral complex refractive index and single scattering albedo data for Icelandic dust. Our results show that the imaginary part of the complex refractive index of Icelandic dust is at the upper end of the range of low-latitude dust. Furthermore, we observed that Icelandic dust is more absorbing towards the near-infrared, which we attribute to its high magnetite content. These findings are important for modeling dust aerosol radiative effects in the Arctic.
Emelie L. Graham, Cheng Wu, David M. Bell, Amelie Bertrand, Sophie L. Haslett, Urs Baltensperger, Imad El Haddad, Radovan Krejci, Ilona Riipinen, and Claudia Mohr
Atmos. Chem. Phys., 23, 7347–7362, https://doi.org/10.5194/acp-23-7347-2023, https://doi.org/10.5194/acp-23-7347-2023, 2023
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The volatility of an aerosol particle is an important parameter for describing its atmospheric lifetime. We studied the volatility of secondary organic aerosols from nitrate-initiated oxidation of three biogenic precursors with experimental methods and model simulations. We saw higher volatility than for the corresponding ozone system, and our simulations produced variable results with different parameterizations which warrant a re-evaluation of the treatment of the nitrate functional group.
Zijun Li, Noora Hyttinen, Miika Vainikka, Olli-Pekka Tikkasalo, Siegfried Schobesberger, and Taina Yli-Juuti
Atmos. Chem. Phys., 23, 6863–6877, https://doi.org/10.5194/acp-23-6863-2023, https://doi.org/10.5194/acp-23-6863-2023, 2023
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The saturation vapor pressure (psat) of low-volatility organic compounds (LVOCs) governs their partitioning between the gas and particle phases. To estimate the psat of selected LVOCs, we performed particle evaporation measurements in a residence time chamber at a temperature setting relevant to atmospheric aerosol formation and conducted state-of-the-art computational calculations. We found good agreement between the experimentally measured and model-estimated psat values for most LVOCs.
Yan Li, Falei Xu, Juan Feng, Mengying Du, Wenjun Song, Chao Li, and Wenjing Zhao
Atmos. Chem. Phys., 23, 6021–6042, https://doi.org/10.5194/acp-23-6021-2023, https://doi.org/10.5194/acp-23-6021-2023, 2023
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There is a significantly negative relationship between boreal winter North Atlantic Oscillation (NAO) and dust aerosols (DAs) in the eastern part of China (30–40°N, 105–120°E), which is not a DA source area but is severely affected by the dust events (DEs). Under the effect of the NAO negative phase, main atmospheric circulation during the DEs is characterized by variation of the transient eddy flux. The work is of reference value to the prediction of DEs and the understanding of their causes.
Ingrid de Almeida Ribeiro, Konrad Meister, and Valeria Molinero
Atmos. Chem. Phys., 23, 5623–5639, https://doi.org/10.5194/acp-23-5623-2023, https://doi.org/10.5194/acp-23-5623-2023, 2023
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Ice formation is a key atmospheric process facilitated by a wide range of aerosols. We present a method to model and interpret ice nucleation experiments and extract the distribution of the potency of nucleation sites. We use the method to optimize the conditions of laboratory sampling and extract distributions of ice nucleation temperatures from bacteria, fungi, and pollen. These reveal unforeseen subpopulations of nuclei in these systems and how they respond to changes in their environment.
Ting Lei, Hang Su, Nan Ma, Ulrich Pöschl, Alfred Wiedensohler, and Yafang Cheng
Atmos. Chem. Phys., 23, 4763–4774, https://doi.org/10.5194/acp-23-4763-2023, https://doi.org/10.5194/acp-23-4763-2023, 2023
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We investigate the hygroscopic behavior of levoglucosan and D-glucose nanoparticles using a nano-HTDMA. There is a weak size dependence of the hygroscopic growth factor of levoglucosan and D-glucose with diameters down to 20 nm, while a strong size dependence of the hygroscopic growth factor of D-glucose has been clearly observed in the size range 6 to 20 nm. The use of the DKA method leads to good agreement with the hygroscopic growth factor of glucose nanoparticles with diameters down to 6 nm.
Lubica Vetráková, Vilém Neděla, Kamila Závacká, Xin Yang, and Dominik Heger
Atmos. Chem. Phys., 23, 4463–4488, https://doi.org/10.5194/acp-23-4463-2023, https://doi.org/10.5194/acp-23-4463-2023, 2023
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Salt aerosols are important to polar atmospheric chemistry and global climate. Therefore, we utilized a unique electron microscope to identify the most suitable conditions for formation of the small salt (CsCl) particles, proxies of the aerosols, from sublimating salty snow. Very low sublimation temperature and low salt concentration are needed for formation of such particles. These observations may help us to better understand polar spring ozone depletion and bromine explosion events.
Xiaohan Li and Ian C. Bourg
Atmos. Chem. Phys., 23, 2525–2556, https://doi.org/10.5194/acp-23-2525-2023, https://doi.org/10.5194/acp-23-2525-2023, 2023
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Aerosol particles with sizes smaller than 50 nm impact cloud formation and precipitation. Representation of this effect is hindered by limited understanding of the properties of liquid water in these particles. Our simulations of aerosol particles containing salt or organic compounds reveal that water enters a less cohesive phase at droplet sizes below 4 nm. This effect causes important deviations from theoretical predictions of aerosol properties, including phase state and hygroscopic growth.
Kristian Klumpp, Claudia Marcolli, Ana Alonso-Hellweg, Christopher H. Dreimol, and Thomas Peter
Atmos. Chem. Phys., 23, 1579–1598, https://doi.org/10.5194/acp-23-1579-2023, https://doi.org/10.5194/acp-23-1579-2023, 2023
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The prerequisites of a particle surface for efficient ice nucleation are still poorly understood. This study compares the ice nucleation activity of two chemically identical but morphologically different minerals (kaolinite and halloysite). We observe, on average, not only higher ice nucleation activities for halloysite than kaolinite but also higher diversity between individual samples. We identify the particle edges as being the most likely site for ice nucleation.
Fabian Mahrt, Carolin Rösch, Kunfeng Gao, Christopher H. Dreimol, Maria A. Zawadowicz, and Zamin A. Kanji
Atmos. Chem. Phys., 23, 1285–1308, https://doi.org/10.5194/acp-23-1285-2023, https://doi.org/10.5194/acp-23-1285-2023, 2023
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Major aerosol types emitted by biomass burning include soot, ash, and charcoal particles. Here, we investigated the ice nucleation activity of 400 nm size-selected particles of two different pyrolyis-derived charcoal types in the mixed phase and cirrus cloud regime. We find that ice nucleation is constrained to cirrus cloud conditions, takes place via pore condensation and freezing, and is largely governed by the particle porosity and mineral content.
Chun Xiong, Xueyan Chen, Xiaolei Ding, Binyu Kuang, Xiangyu Pei, Zhengning Xu, Shikuan Yang, Huan Hu, and Zhibin Wang
Atmos. Chem. Phys., 22, 16123–16135, https://doi.org/10.5194/acp-22-16123-2022, https://doi.org/10.5194/acp-22-16123-2022, 2022
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Water surface tension is applied widely in current aerosol–cloud models but could be inappropriate in the presence of atmospheric surfactants. With cloud condensation nuclei (CCN) activity and atomic force microscopy (AFM) measurement results of mixed inorganic salt and dicarboxylic acid particles, we concluded that surface tension reduction and phase state should be carefully considered in aerosol–cloud interactions. Our results could help to decease uncertainties in climate models.
Bernadette Rosati, Sini Isokääntä, Sigurd Christiansen, Mads Mørk Jensen, Shamjad P. Moosakutty, Robin Wollesen de Jonge, Andreas Massling, Marianne Glasius, Jonas Elm, Annele Virtanen, and Merete Bilde
Atmos. Chem. Phys., 22, 13449–13466, https://doi.org/10.5194/acp-22-13449-2022, https://doi.org/10.5194/acp-22-13449-2022, 2022
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Sulfate aerosols have a strong influence on climate. Due to the reduction in sulfur-based fossil fuels, natural sulfur emissions play an increasingly important role. Studies investigating the climate relevance of natural sulfur aerosols are scarce. We study the water uptake of such particles in the laboratory, demonstrating a high potential to take up water and form cloud droplets. During atmospheric transit, chemical processing affects the particles’ composition and thus their water uptake.
Kanishk Gohil, Chun-Ning Mao, Dewansh Rastogi, Chao Peng, Mingjin Tang, and Akua Asa-Awuku
Atmos. Chem. Phys., 22, 12769–12787, https://doi.org/10.5194/acp-22-12769-2022, https://doi.org/10.5194/acp-22-12769-2022, 2022
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The Hybrid Activity Model (HAM) is a promising new droplet growth model that can be potentially used for the analysis of any type of atmospheric compound. HAM may potentially improve the representation of hygroscopicity of organic aerosols in large-scale global climate models (GCMs), hence reducing the uncertainties in the climate forcing due to the aerosol indirect effect.
Charbel Harb and Hosein Foroutan
Atmos. Chem. Phys., 22, 11759–11779, https://doi.org/10.5194/acp-22-11759-2022, https://doi.org/10.5194/acp-22-11759-2022, 2022
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A model representation of lake spray aerosol (LSA) ejection from freshwater breaking waves is crucial for understanding their climatic and public health impacts. We develop an LSA emission parameterization and implement it in an atmospheric model to investigate Great Lakes surface emissions. We find that the same breaking wave is likely to produce fewer aerosols in freshwater than in saltwater and that Great Lakes emissions influence the regional aerosol burden and can reach the cloud layer.
Runlong Cai, Ella Häkkinen, Chao Yan, Jingkun Jiang, Markku Kulmala, and Juha Kangasluoma
Atmos. Chem. Phys., 22, 11529–11541, https://doi.org/10.5194/acp-22-11529-2022, https://doi.org/10.5194/acp-22-11529-2022, 2022
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The influences of new particle formation on the climate and air quality are governed by particle survival, which has been under debate due to uncertainties in the coagulation sink. Here we measure the coagulation coefficient of sub-10 nm particles and demonstrate that collisions between the freshly nucleated and background particles can effectively lead to coagulation. We further show that the effective coagulation sink is consistent with the new particle formation measured in urban Beijing.
Lamei Shi, Jiahua Zhang, Da Zhang, Jingwen Wang, Xianglei Meng, Yuqin Liu, and Fengmei Yao
Atmos. Chem. Phys., 22, 11255–11274, https://doi.org/10.5194/acp-22-11255-2022, https://doi.org/10.5194/acp-22-11255-2022, 2022
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Dust impacts climate and human life. Analyzing the interdecadal change in dust activity and its influence factors is crucial for disaster mitigation. Based on a linear regression method, this study revealed the interdecadal variability of relationships between ENSO and dust over northwestern South Asia from 1982 to 2014 and analyzed the effects of atmospheric factors on this interdecadal variability. The result sheds new light on numerical simulation involving the interdecadal variation of dust.
Bighnaraj Sarangi, Darrel Baumgardner, Benjamin Bolaños-Rosero, and Olga L. Mayol-Bracero
Atmos. Chem. Phys., 22, 9647–9661, https://doi.org/10.5194/acp-22-9647-2022, https://doi.org/10.5194/acp-22-9647-2022, 2022
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Here, the fluorescent characteristics and cloud-forming efficiency of aerosols at an urban site in Puerto Rico are discussed. The results from this pilot study highlight the capabilities of ultraviolet-induced fluorescence (UV-IF) measurements for characterizing the properties of fluorescing aerosol particles, as they relate to the daily evolution of primary biological aerosol particles. This work has established a database of measurements on which future, longer-term studies will be initiated.
Rani Jeong, Joseph Lilek, Andreas Zuend, Rongshuang Xu, Man Nin Chan, Dohyun Kim, Hi Gyu Moon, and Mijung Song
Atmos. Chem. Phys., 22, 8805–8817, https://doi.org/10.5194/acp-22-8805-2022, https://doi.org/10.5194/acp-22-8805-2022, 2022
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In this study, the viscosities of particles of sucrose–H2O, AS–H2O, and sucrose–AS–H2O for OIRs of 4:1, 1:1, and 1:4 for decreasing RH, were quantified by poke-and-flow and bead-mobility techniques at 293 ± 1 K. Based on the viscosity results, the particles of binary and ternary systems ranged from liquid to semisolid, and even the solid state depending on the RH. Moreover, we compared the measured viscosities of ternary systems to the predicted viscosities with excellent agreement.
Minxia Shen, Kin Fai Ho, Wenting Dai, Suixin Liu, Ting Zhang, Qiyuan Wang, Jingjing Meng, Judith C. Chow, John G. Watson, Junji Cao, and Jianjun Li
Atmos. Chem. Phys., 22, 7489–7504, https://doi.org/10.5194/acp-22-7489-2022, https://doi.org/10.5194/acp-22-7489-2022, 2022
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Looking at characteristics and δ13C compositions of dicarboxylic acids and related compounds in BB aerosols, we used a combined combustion and aging system to generate fresh and aged aerosols from burning straw. The results showed the emission factors (EFaged) of total diacids of aging experiments were around an order of magnitude higher than EFfresh. This meant that dicarboxylic acids are involved with secondary photochemical processes in the atmosphere rather than primary emissions from BB.
Jonas K. F. Jakobsson, Deepak B. Waman, Vaughan T. J. Phillips, and Thomas Bjerring Kristensen
Atmos. Chem. Phys., 22, 6717–6748, https://doi.org/10.5194/acp-22-6717-2022, https://doi.org/10.5194/acp-22-6717-2022, 2022
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Long-lived cold-layer clouds at subzero temperatures are observed to be remarkably persistent in their generation of ice particles and snow precipitation. There is uncertainty about why this is so. This motivates the present lab study to observe the long-term ice-nucleating ability of aerosol samples from the real troposphere. Time dependence of their ice nucleation is observed to be weak in lab experiments exposing the samples to isothermal conditions for up to about 10 h.
Kunfeng Gao, Chong-Wen Zhou, Eszter J. Barthazy Meier, and Zamin A. Kanji
Atmos. Chem. Phys., 22, 5331–5364, https://doi.org/10.5194/acp-22-5331-2022, https://doi.org/10.5194/acp-22-5331-2022, 2022
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Incomplete combustion of fossil fuel produces carbonaceous particles called soot. These particles can affect cloud formation by acting as centres for droplet or ice formation. The atmospheric residence time of soot particles is of the order of days to weeks, which can result in them becoming coated by various trace species in the atmosphere such as acids. In this study, we quantify the cirrus cloud-forming ability of soot particles coated with the atmospherically ubiquitous sulfuric acid.
Kunfeng Gao, Franz Friebel, Chong-Wen Zhou, and Zamin A. Kanji
Atmos. Chem. Phys., 22, 4985–5016, https://doi.org/10.5194/acp-22-4985-2022, https://doi.org/10.5194/acp-22-4985-2022, 2022
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Soot particles impact cloud formation and radiative properties in the upper atmosphere where aircraft emit carbonaceous particles. We use cloud chambers to mimic the upper atmosphere temperature and humidity to test the influence of the morphology of the soot particles on ice cloud formation. For particles larger than 200 nm, the compacted (densified) samples have a higher affinity for ice crystal formation in the cirrus regime than the fluffy (un-compacted) soot particles of the same sample.
Joel Kuula, Hilkka Timonen, Jarkko V. Niemi, Hanna E. Manninen, Topi Rönkkö, Tareq Hussein, Pak Lun Fung, Sasu Tarkoma, Mikko Laakso, Erkka Saukko, Aino Ovaska, Markku Kulmala, Ari Karppinen, Lasse Johansson, and Tuukka Petäjä
Atmos. Chem. Phys., 22, 4801–4808, https://doi.org/10.5194/acp-22-4801-2022, https://doi.org/10.5194/acp-22-4801-2022, 2022
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Modern and up-to-date policies and air quality management strategies are instrumental in tackling global air pollution. As the European Union is preparing to revise Ambient Air Quality Directive 2008/50/EC, this paper initiates discussion on selected features of the directive that we believe would benefit from a reassessment. The scientific community has the most recent and deepest understanding of air pollution; thus, its contribution is essential.
Yu Wang, Aristeidis Voliotis, Dawei Hu, Yunqi Shao, Mao Du, Ying Chen, Judith Kleinheins, Claudia Marcolli, M. Rami Alfarra, and Gordon McFiggans
Atmos. Chem. Phys., 22, 4149–4166, https://doi.org/10.5194/acp-22-4149-2022, https://doi.org/10.5194/acp-22-4149-2022, 2022
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Aerosol water uptake plays a key role in atmospheric physicochemical processes. We designed chamber experiments on aerosol water uptake of secondary organic aerosol (SOA) from mixed biogenic and anthropogenic precursors with inorganic seed. Our results highlight this chemical composition influences the reconciliation of the sub- and super-saturated water uptake, providing laboratory evidence for understanding the chemical controls of water uptake of the multi-component aerosol.
Shuang Han, Juan Hong, Qingwei Luo, Hanbing Xu, Haobo Tan, Qiaoqiao Wang, Jiangchuan Tao, Yaqing Zhou, Long Peng, Yao He, Jingnan Shi, Nan Ma, Yafang Cheng, and Hang Su
Atmos. Chem. Phys., 22, 3985–4004, https://doi.org/10.5194/acp-22-3985-2022, https://doi.org/10.5194/acp-22-3985-2022, 2022
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We present the hygroscopicity of 23 organic species with different physicochemical properties using a hygroscopicity tandem differential mobility analyzer (HTDMA) and compare the results with previous studies. Based on the hygroscopicity parameter κ, the influence of different physicochemical properties that potentially drive hygroscopicity, such as the functionality, water solubility, molar volume, and O : C ratio of organics, are examined separately.
Kimmo Korhonen, Thomas Bjerring Kristensen, John Falk, Vilhelm B. Malmborg, Axel Eriksson, Louise Gren, Maja Novakovic, Sam Shamun, Panu Karjalainen, Lassi Markkula, Joakim Pagels, Birgitta Svenningsson, Martin Tunér, Mika Komppula, Ari Laaksonen, and Annele Virtanen
Atmos. Chem. Phys., 22, 1615–1631, https://doi.org/10.5194/acp-22-1615-2022, https://doi.org/10.5194/acp-22-1615-2022, 2022
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We investigated the ice-nucleating abilities of particulate emissions from a modern diesel engine using the portable ice-nuclei counter SPIN, a continuous-flow diffusion chamber instrument. Three different fuels were studied without blending, including fossil diesel and two renewable fuels, testing different emission aftertreatment systems and photochemical aging. We found that the diesel emissions were inefficient ice nuclei, and aging had no or little effect on their ice-nucleating abilities.
Noora Hyttinen, Iida Pullinen, Aki Nissinen, Siegfried Schobesberger, Annele Virtanen, and Taina Yli-Juuti
Atmos. Chem. Phys., 22, 1195–1208, https://doi.org/10.5194/acp-22-1195-2022, https://doi.org/10.5194/acp-22-1195-2022, 2022
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Accurate saturation vapor pressure estimates of atmospherically relevant organic compounds are critical for modeling secondary organic aerosol (SOA) formation. We investigated vapor pressures of highly oxygenated SOA constituents using state-of-the-art computational and experimental methods. We found a good agreement between low and extremely low vapor pressures estimated using the two methods, and the smallest molecules detected in our experiment were likely products of thermal decomposition.
Dawei Hu, M. Rami Alfarra, Kate Szpek, Justin M. Langridge, Michael I. Cotterell, Claire Belcher, Ian Rule, Zixia Liu, Chenjie Yu, Yunqi Shao, Aristeidis Voliotis, Mao Du, Brett Smith, Greg Smallwood, Prem Lobo, Dantong Liu, Jim M. Haywood, Hugh Coe, and James D. Allan
Atmos. Chem. Phys., 21, 16161–16182, https://doi.org/10.5194/acp-21-16161-2021, https://doi.org/10.5194/acp-21-16161-2021, 2021
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Here, we developed new techniques for investigating these properties in the laboratory and applied these to BC and BrC from different sources, including diesel exhaust, inverted propane flame and wood combustion. These have allowed us to quantify the changes in shape and chemical composition of different soots according to source and variables such as the moisture content of wood.
Mariam Fawaz, Anita Avery, Timothy B. Onasch, Leah R. Williams, and Tami C. Bond
Atmos. Chem. Phys., 21, 15605–15618, https://doi.org/10.5194/acp-21-15605-2021, https://doi.org/10.5194/acp-21-15605-2021, 2021
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Biomass burning is responsible for 90 % of the emissions of primary organic aerosols to the atmosphere. Emissions from biomass burning sources are considered chaotic. In this work, we developed a controlled experimental approach to understand the controlling factors in emission. Our results showed that emissions are repeatable and deterministic and that emissions from wood can be constrained.
Soleil E. Worthy, Anand Kumar, Yu Xi, Jingwei Yun, Jessie Chen, Cuishan Xu, Victoria E. Irish, Pierre Amato, and Allan K. Bertram
Atmos. Chem. Phys., 21, 14631–14648, https://doi.org/10.5194/acp-21-14631-2021, https://doi.org/10.5194/acp-21-14631-2021, 2021
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We studied the effect of (NH4)2SO4 on the immersion freezing of non-mineral dust ice-nucleating substances (INSs) and mineral dusts. (NH4)2SO4 had no effect on the median freezing temperature of 9 of the 10 tested non-mineral dust INSs, slightly decreased that of the other, and increased that of all the mineral dusts. The difference in the response of mineral dust and non-mineral dust INSs to (NH4)2SO4 suggests that they nucleate ice and/or interact with (NH4)2SO4 via different mechanisms.
Robert Wagner, Luisa Ickes, Allan K. Bertram, Nora Els, Elena Gorokhova, Ottmar Möhler, Benjamin J. Murray, Nsikanabasi Silas Umo, and Matthew E. Salter
Atmos. Chem. Phys., 21, 13903–13930, https://doi.org/10.5194/acp-21-13903-2021, https://doi.org/10.5194/acp-21-13903-2021, 2021
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Sea spray aerosol particles are a mixture of inorganic salts and organic matter from phytoplankton organisms. At low temperatures in the upper troposphere, both inorganic and organic constituents can induce the formation of ice crystals and thereby impact cloud properties and climate. In this study, we performed experiments in a cloud simulation chamber with particles produced from Arctic seawater samples to quantify the relative contribution of inorganic and organic species in ice formation.
Matthew Ozon, Dominik Stolzenburg, Lubna Dada, Aku Seppänen, and Kari E. J. Lehtinen
Atmos. Chem. Phys., 21, 12595–12611, https://doi.org/10.5194/acp-21-12595-2021, https://doi.org/10.5194/acp-21-12595-2021, 2021
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Measuring the rate at which aerosol particles are formed is of importance for understanding climate change. We present an analysis method based on Kalman smoothing, which retrieves new particle formation and growth rates from size-distribution measurements. We apply it to atmospheric simulation chamber experiments and show that it agrees well with traditional methods. In addition, it provides reliable uncertainty estimates, and we suggest instrument design optimisation for signal processing.
Yu Wang, Aristeidis Voliotis, Yunqi Shao, Taomou Zong, Xiangxinyue Meng, Mao Du, Dawei Hu, Ying Chen, Zhijun Wu, M. Rami Alfarra, and Gordon McFiggans
Atmos. Chem. Phys., 21, 11303–11316, https://doi.org/10.5194/acp-21-11303-2021, https://doi.org/10.5194/acp-21-11303-2021, 2021
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Aerosol phase behaviour plays a profound role in atmospheric physicochemical processes. We designed dedicated chamber experiments to study the phase state of secondary organic aerosol from biogenic and anthropogenic mixed precursors. Our results highlight the key role of the organic–inorganic ratio and relative humidity in phase state, but the sources and organic composition are less important. The result provides solid laboratory evidence for understanding aerosol phase in a complex atmosphere.
Ana A. Piedehierro, André Welti, Angela Buchholz, Kimmo Korhonen, Iida Pullinen, Ilkka Summanen, Annele Virtanen, and Ari Laaksonen
Atmos. Chem. Phys., 21, 11069–11078, https://doi.org/10.5194/acp-21-11069-2021, https://doi.org/10.5194/acp-21-11069-2021, 2021
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Ice crystals in cirrus clouds contain particles that start ice formation. We study whether particles forming above boreal forests can help in the making of cirrus clouds and if the water content in the particles affects this property. In the laboratory, we made boreal-forest-like particles and cooled and humidified them to measure whether an ice crystal develops. We found that only when dry can these particles form an ice crystal but no better than solution droplets.
Young-Chul Song, Joseph Lilek, Jae Bong Lee, Man Nin Chan, Zhijun Wu, Andreas Zuend, and Mijung Song
Atmos. Chem. Phys., 21, 10215–10228, https://doi.org/10.5194/acp-21-10215-2021, https://doi.org/10.5194/acp-21-10215-2021, 2021
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We report viscosity of binary mixtures of organic material / H2O and inorganic salts / H2O, as well as ternary mixtures of organic material / inorganic salts/ H2O, over the atmospheric relative humidity (RH) range. The viscosity measurements indicate that the studied mixed organic–inorganic particles range in phase state from liquid to semi-solid or even solid across the atmospheric RH range at a temperature of 293 K.
Cited articles
Altaf, M. B. and Freedman, M. A.: Effect of Drying Rate on Aerosol Particle
Morphology, J. Phys. Chem. Lett., 8, 3613–3618, https://doi.org/10.1021/acs.jpclett.7b01327, 2017.
Altaf, M. B., Dutcher, D. D., Raymond, T. M., and Freedman, M. A.: Effect of
Particle Morphology on Cloud Condensation Nuclei Activity, ACS Earth Space
Chem., 2, 634–639, https://doi.org/10.1021/acsearthspacechem.7b00146, 2018.
Bertram, A. K., Martin, S. T., Hanna, S. J., Smith, M. L., Bodsworth, A.,
Chen, Q., Kuwata, M., Liu, A., You, Y., and Zorn, S. R.: Predicting the
Relative Humidities of Liquid-Liquid Phase Separation, Efflorescence, and
Deliquescence of Mixed Particles of Ammonium Sulfate, Organic Material, and
Water Using the Organic-to-Sulfate Mass Ratio of the Particle and the
Oxygen-to-Carbon Elemental Ratio of the Organic Component, Atmos. Chem.
Phys., 11, 10995–11006, https://doi.org/10.5194/acp-11-10995-2011, 2011.
Boistelle, R. and Astier, J. P.: Crystallization Mechanisms in Solution, J.
Cryst. Growth, 90, 14–30, https://doi.org/10.1016/0022-0248(88)90294-1, 1988.
Bruggemann, M., Xu, R. S., Tilgner, A., Kwong, K. C., Mutzel, A., Poon, H.
Y., Otto, T., Schaefer, T., Poulain, L., Chan, M. N., and Herrmann, H.:
Organosulfates in Ambient Aerosol: State of Knowledge and Future Research
Directions on Formation, Abundance, Fate, and Importance, Environ. Sci.
Technol., 54, 3767–3782, https://doi.org/10.1021/acs.est.9b06751, 2020.
Cheng, M. Q. and Kuwata, M.: Development of the Low-Temperature
Hygroscopicity Tandem Differential Mobility Analyzer (Low-T HTDMA) and its
Application to (NH4)2SO4 and NaCl Particles, J. Aerosol Sci., 168, 106111, https://doi.org/10.1016/j.jaerosci.2022.106111, 2023.
Choi, M. Y. and Chan, C. K.: The Effects of Organic Species on the Hygroscopic Behaviors of Inorganic Aerosols, Environ. Sci. Technol., 36,
2422–2428, https://doi.org/10.1021/es0113293, 2002.
Ciobanu, V. G., Marcolli, C., Krieger, U. K., Weers, U., and Peter, T.:
Liquid-Liquid Phase Separation in Mixed Organic/Inorganic Aerosol Particles,
J. Phys. Chem. A, 113, 10966–10978, https://doi.org/10.1021/jp905054d, 2009.
Fountoukis, C. and Nenes, A.: ISORROPIA II: a computationally efficient
thermodynamic equilibrium model for
K+–Ca
Freedman, M. A.: Liquid-Liquid Phase Separation in Supermicrometer and
Submicrometer Aerosol Particles, Acc. Chem. Res., 53, 1102–1110,
https://doi.org/10.1021/acs.accounts.0c00093, 2020.
Ghorai, S., Wang, B. B., Tivanski, A., and Laskin, A.: Hygroscopic Properties of Internally Mixed Particles Composed of NaCl and Water-Soluble Organic Acids, Environ. Sci. Technol., 48, 2234–2241, https://doi.org/10.1021/es404727u, 2014.
Griffin, R. J., Nguyen, K., Dabdub, D., and Seinfeld, J. H.: A coupled
hydrophobic-hydrophilic model for predicting secondary organic aerosol
formation, J. Atmos. Chem., 44, 171–190, https://doi.org/10.1023/A:1022436813699, 2003.
Guo, L. Y., Peng, C., Zong, T. M., Gu, W. J., Ma, Q. X., Wu, Z. J., Wang, Z., Ding, X., Hu, M., Wang, X. M., and Tang, M. J.: Comprehensive Characterization of Hygroscopic Properties of Methanesulfonates, Atmos.
Environ., 224, 117349, https://doi.org/10.1016/j.atmosenv.2020.117349, 2020.
Ho, K. F., Lee, S. C., Ho, S. S. H., Kawamura, K., Tachibana, E., Cheng, Y.,
and Zhu, T.: Dicarboxylic acids, ketocarboxylic acids, α-dicarbonyls, fatty acids, and benzoic acid in urban aerosols collected during the 2006 Campaign of Air Quality Research in Beijing (CAREBeijing-2006), J. Geophys. Res.-Atmos., 115, D19312, https://doi.org/10.1029/2009jd013304, 2010.
Hyder, M., Genberg, J., Sandahl, M., Swietlicki, E., and Jönsson, J. Å.: Yearly trend of dicarboxylic acids in organic aerosols from south of
Sweden and source attribution, Atmos. Environ., 57, 197–204,
https://doi.org/10.1016/j.atmosenv.2012.04.027, 2012.
Kirpes, R. M., Lei, Z. Y., Fraund, M., Gunsch, M. J., May, N. W., Barrett,
T. E., Moffett, C. E., Schauer, A. J., Alexander, B., Upchurch, L. M., China, S., Quinn, P. K., Moffet, R. C., Laskin, A., Sheesley, R. J., Pratt, K. A., and Ault, A. P.: Solid organic-coated ammonium sulfate particles at high relative humidity in the summertime Arctic atmosphere, P. Natl. Acad. Sci. USA, 119, e2104496119, https://doi.org/10.1073/pnas.2104496119, 2022.
Kwamena, N. O. A., Buajarern, J., and Reid, J. P.: Equilibrium Morphology of
Mixed Organic/Inorganic/Aqueous Aerosol Droplets: Investigating the Effect
of Relative Humidity and Surfactants, J. Phys. Chem. A, 114, 5787–5795,
https://doi.org/10.1021/jp1003648, 2010.
Lambert, F., Kug, J. S., Park, R. J., Mahowald, N., Winckler, G., Abe-Ouchi,
A., O'Ishi, R., Takemura, T., and Lee, J. H.: The role of mineral-dust aerosols in polar temperature amplification, Nat. Clim. Change, 3, 487–491,
https://doi.org/10.1038/Nclimate1785, 2013.
Laskin, A., Cowin, J. P., and Iedema, M. J.: Analysis of Individual Environmental Particles using Modern Methods of Electron Microscopy and
X-ray Microanalysis, J. Electron. Spectrosc. Relat. Phenom., 150, 260–274,
https://doi.org/10.1016/j.elspec.2005.06.008, 2006.
Laskina, O., Morris, H. S., Grandquist, J. R., Qiu, Z., Stone, E. A.,
Tivanski, A. V., and Grassian, V. H.: Size Matters in the Water Uptake and
Hygroscopic Growth of Atmospherically Relevant Multicomponent Aerosol
Particles, J. Phys. Chem. A, 119, 4489–4497, https://doi.org/10.1021/jp510268p, 2015.
Li, W. J., Shao, L. Y., Zhang, D. Z., Ro, C. U., Hu, M., Bi, X. H., Geng, H., Matsuki, A., Niu, H. Y., and Chen, J. M.: A review of single aerosol particle studies in the atmosphere of East Asia: morphology, mixing state, source, and heterogeneous reactions, J. Clean. Product., 112, 1330–1349,
https://doi.org/10.1016/j.jclepro.2015.04.050, 2016.
Li, W. J., Teng, X. M., Chen, X. Y., Liu, L., Xu, L., Zhang, J., Wang, Y. Y., Zhang, Y., and Shi, Z. B.: Organic Coating Reduces Hygroscopic Growth of
Phase-Separated Aerosol Particles, Environ. Sci. Technol., 55, 16339–16346,
https://doi.org/10.1021/acs.est.1c05901, 2021.
Ma, S. S., Pang, S. F., Li, J., and Zhang, Y. H.: A review of efflorescence
kinetics studies on atmospherically relevant particles, Chemosphere, 277,
130320, https://doi.org/10.1016/j.chemosphere.2021.130320, 2021.
Martin, S. T.: Phase Transitions of Aqueous Atmospheric Particles, Chem. Rev., 100, 3403–3453, https://doi.org/10.1021/cr990034t, 2000.
Metzger, S., Dentener, F., Krol, M., Jeuken, A., and Lelieveld, J.:
Gas/aerosol partitioning 2. Global modeling results, J. Geophys. Res.-Atmos., 107, ACH 17-1–ACH 17-23, https://doi.org/10.1029/2001jd001103, 2002a.
Metzger, S., Dentener, F., Pandis, S., and Lelieveld, J.: Gas/aerosol
partitioning 1. A computationally efficient model, J. Geophys. Res.-Atmos., 107, 4312, https://doi.org/10.1029/2001jd001102, 2002b.
Myhre, G., Bellouin, N., Berglen, T. F., Berntsen, T. K., Boucher, O.,
Grini, A., Isaksen, I. S. A., Johnsrud, M., Mishchenko, M. I., Stordal, F.,
and Tanre, D.: Comparison of the radiative properties and direct radiative
effect of aerosols from a global aerosol model and remote sensing data over
ocean, Tellus B, 59, 115–129, https://doi.org/10.1111/j.1600-0889.2006.00238.x, 2007.
Nandy, L., Yao, Y., Zheng, Z. H., and Riemer, N.: Water uptake and optical
properties of mixed organic-inorganic particles, Aerosol Sci. Tech., 55,
1398–1413, https://doi.org/10.1080/02786826.2021.1966378, 2021.
Nguyen, Q. T., Kjær, K. H., Kling, K. I., Boesen, T., and Bilde, M.:
Impact of Fatty Acid Coating on the CCN Activity of Sea Salt Particles,
Tellus B, 69, 1304064, https://doi.org/10.1080/16000889.2017.1304064, 2017.
Noziere, B.: Don't Forget the Surface, Science, 351, 1396–1397,
https://doi.org/10.1126/science.aaf3253, 2016.
O'Brien, R. E., Wang, B. B., Kelly, S. T., Lundt, N., You, Y., Bertram, A.
K., Leone, S. R., Laskin, A., and Gilles, M. K.: Liquid-Liquid Phase Separation in Aerosol Particles: Imaging at the Nanometer Scale, Environ.
Sci. Technol., 49, 4995–5002, https://doi.org/10.1021/acs.est.5b00062, 2015.
Ohno, P. E., Qin, Y. M., Ye, J. H., Wang, J. F., Bertram, A. K., and Martin,
S. T.: Fluorescence Aerosol Flow Tube Spectroscopy to Detect Liquid-Liquid
Phase Separation, ACS Earth Space Chem., 5, 1223–1232,
https://doi.org/10.1021/acsearthspacechem.1c00061, 2021.
Ohno, P. E., Brandao, L., Rainone, E. M., Aruffo, E., Wang, J. F., Qin, Y.
M., and Martin, S. T.: Size Dependence of Liquid-Liquid Phase Separation by
in Situ Study of Flowing Submicron Aerosol Particles, J. Phys. Chem. A, 127,
2967–2974, https://doi.org/10.1021/acs.jpca.2c08224, 2023.
Onasch, T. B., Siefert, R. L., Brooks, S. D., Prenni, A. J., Murray, B.,
Wilson, M. A., and Tolbert, M. A.: Infrared Spectroscopic Study of The
Deliquescence and Efflorescence of Ammonium Sulfate Aerosol as a Function of
Temperature, J. Geophys. Res.-Atmos., 104, 21317–21326, https://doi.org/10.1029/1999jd900384, 1999.
Ott, E. J. E. and Freedman, M. A.: Influence of Ions on the Size Dependent
Morphology of Aerosol Particles, ACS Earth Space Chem., 5, 2320–2328,
https://doi.org/10.1021/acsearthspacechem.1c00210, 2021.
Ott, E. J. E., Kucinski, T. M., Dawson, J. N., and Freedman, M. A.: Use of
Transmission Electron Microscopy for Analysis of Aerosol Particles and
Strategies for Imaging Fragile Particles, Anal. Chem., 93, 11347–11356,
https://doi.org/10.1021/acs.analchem.0c05225, 2021.
Peng, C., Chan, M. N., and Chan, C. K.: The Hygroscopic Properties of
Dicarboxylic and Multifunctional Acids: Measurements and UNIFAC Predictions,
Environ. Sci. Technol., 35, 4495–4501, https://doi.org/10.1021/es0107531, 2001.
Peng, C., Jing, B., Guo, Y. C., Zhang, Y. H., and Ge, M. F.: Hygroscopic
Behavior of Multicomponent Aerosols Involving NaCl and Dicarboxylic Acids,
J. Phys. Chem. A, 120, 1029–1038, https://doi.org/10.1021/acs.jpca.5b09373, 2016.
Peng, C., Chen, L., and Tang, M.: A Database for Deliquescence and
Efflorescence Relative Humidities of Compounds with Atmospheric Relevance,
Fundam. Res., 2, 578–587, https://doi.org/10.1016/j.fmre.2021.11.021, 2022.
Petters, M. D. and Kreidenweis, S. M.: A single parameter representation of
hygroscopic growth and cloud condensation nucleus activity, Atmos. Chem.
Phys., 7, 1961–1971, https://doi.org/10.5194/acp-7-1961-2007, 2007.
Pöhlker, C., Saturno, J., Krüger, M. L., Förster, J. D., Weigand, M., Wiedemann, K. T., Bechtel, M., Artaxo, P., and Andreae, M. O.: Efflorescence upon Humidification? X-ray Microspectroscopic in situ Observation of Changes in Aerosol Microstructure and Phase State upon Hydration, Geophys. Res. Lett., 41, 3681–3689, https://doi.org/10.1002/2014gl059409, 2014.
Pöschl, U.: Atmospheric Aerosols: Composition, Transformation, Climate
and Health Effects, Angew. Chem. Int. Ed., 44, 7520–7540,
https://doi.org/10.1002/anie.200501122, 2005.
Posfai, M., Axisa, D., Tompa, E., Freney, E., Bruintjes, R., and Buseck, P.
R.: Interactions of Mineral Dust with Pollution and Clouds: An Individual-Particle TEM Study of Atmospheric Aerosol from Saudi Arabia,
Atmos. Res., 122, 347–361, https://doi.org/10.1016/j.atmosres.2012.12.001, 2013.
Pye, H. O. T., Murphy, B. N., Xu, L., Ng, N. L., Carlton, A. G., Guo, H. Y.,
Weber, R., Vasilakos, P., Appel, K. W., Budisulistiorini, S. H., Surratt, J.
D., Nenes, A., Hu, W. W., Jimenez, J. L., Isaacman-VanWertz, G., Misztal, P.
K., and Goldstein, A. H.: On the implications of aerosol liquid water and
phase separation for organic aerosol mass, Atmos. Chem. Phys., 17, 343–369,
https://doi.org/10.5194/acp-17-343-2017, 2017.
Reed, N. W., Wing, B. A., Tolbert, M. A., and Browne, E. C.: Trace H2S
Promotes Organic Aerosol Production and Organosulfur Compound Formation in
Archean Analog Haze Photochemistry Experiments, Geophys. Res. Lett., 49,
e2021GL097032, https://doi.org/10.1029/2021GL097032, 2022.
Riemer, N., Ault, A. P., West, M., Craig, R. L., and Curtis, J. H.: Aerosol
Mixing State: Measurements, Modeling, and Impacts, Rev. Geophys., 57, 187–249, https://doi.org/10.1029/2018rg000615, 2019.
Römpp, A., Winterhalter, R., and Moortgat, G. K.: Oxodicarboxylic acids
in atmospheric aerosol particles, Atmos. Environ., 40, 6846–6862,
https://doi.org/10.1016/j.atmosenv.2006.05.053, 2006.
Roy, P., Mael, L. E., Makhnenko, I., Martz, R., Grassian, V. H., and Dutcher, C. S.: Temperature-Dependent Phase Transitions of Aqueous Aerosol Droplet Systems in Microfluidic Traps, ACS Earth Space Chem., 4, 1527–1539,
https://doi.org/10.1021/acsearthspacechem.0c00114, 2020.
Ruehl, C. R. and Wilson, K. R.: Surface Organic Monolayers Control the
Hygroscopic Growth of Submicrometer Particles at High Relative Humidity, J.
Phys. Chem. A, 118, 3952–3966, https://doi.org/10.1021/jp502844g, 2014.
Ruehl, C. R., Davies, J. F., and Wilson, K. R.: An Interfacial Mechanism for
Cloud Droplet Formation on Organic Aerosols, Science, 351, 1447–1450,
https://doi.org/10.1126/science.aad4889, 2016.
Shiraiwa, M., Zuend, A., Bertram, A. K., and Seinfeld, J. H.: Gas-Particle
Partitioning of Atmospheric Aerosols: Interplay of Physical State, Non-Ideal
Mixing and Morphology, Phys. Chem. Chem. Phys., 15, 11441–11453,
https://doi.org/10.1039/c3cp51595h, 2013.
Song, M., Marcolli, C., Krieger, U. K., Zuend, A., and Peter, T.: Liquid-Liquid Phase Separation and Morphology of Internally Mixed Dicarboxylic Acids/Ammonium Sulfate/Water Particles, Atmos. Chem. Phys., 12,
2691–2712, https://doi.org/10.5194/acp-12-2691-2012, 2012a.
Song, M., Marcolli, C., Krieger, U. K., Zuend, A., and Peter, T.: Liquid-Liquid Phase Separation in Aerosol Particles: Dependence on O:C, Organic Functionalities, and Compositional Complexity, Geophys. Res. Lett., 39, L19801, https://doi.org/10.1029/2012gl052807, 2012b.
Song, M., Maclean, A. M., Huang, Y. Z., Smith, N. R., Blair, S. L., Laskin,
J., Laskin, A., DeRieux, W. S. W., Li, Y., Shiraiwa, M., Nizkorodov, S. A.,
and Bertram, A. K.: Liquid-Liquid Phase Separation and Viscosity within
Secondary Organic Aerosol Generated from Diesel Fuel Vapors, Atmos. Chem.
Phys., 19, 12515–12529, https://doi.org/10.5194/acp-19-12515-2019, 2019.
Song, M. J., Liu, P. F., Martin, S. T., and Bertram, A. K.: Liquid-Liquid
Phase Separation in Particles Containing Secondary Organic Material Free of
Inorganic Salts, Atmos. Chem. Phys., 17, 11261–11271,
https://doi.org/10.5194/acp-17-11261-2017, 2017.
Stewart, D. J., Cai, C., Nayler, J., Preston, T. C., Reid, J. P., Krieger,
U. K., Marcolli, C., and Zhang, Y. H.: Liquid-Liquid Phase Separation in
Mixed Organic/Inorganic Single Aqueous Aerosol Droplets, J. Phys. Chem. A,
119, 4177–4190, https://doi.org/10.1021/acs.jpca.5b01658, 2015.
Takahama, S., Pathak, R. K., and Pandis, S. N.: Efflorescence Transitions of
Ammonium Sulfate Particles Coated with Secondary Organic Aerosol, Environ.
Sci. Technol., 41, 2289–2295, https://doi.org/10.1021/es0619915, 2007.
Ting, Y. C., Mitchell, E. J. S., Allan, J. D., Liu, D. T., Spracklen, D. V.,
Williams, A., Jones, J. M., Lea-Langton, A. R., McFiggans, G., and Coe, H.:
Mixing State of Carbonaceous Aerosols of Primary Emissions from “Improved”
African Cookstoves, Environ. Sci. Technol., 52, 10134–10143,
https://doi.org/10.1021/acs.est.8b00456, 2018.
Tolocka, M. P. and Turpin, B.: Contribution of Organosulfur Compounds to
Organic Aerosol Mass, Environ. Sci. Technol., 46, 7978–7983,
https://doi.org/10.1021/es300651v, 2012.
Tong, Y. K., Meng, X. X. Y., Zhou, B., Sun, R., Wu, Z. J., Hu, M., and Ye, A. P.: Detecting the pH-dependent liquid-liquid phase separation of single
levitated aerosol microdroplets via laser tweezers-Raman spectroscopy, Front. Phys., 10, 969921, https://doi.org/10.3389/fphy.2022.969921, 2022.
Unga, F., Choel, M., Derimian, Y., Deboudt, K., Dubovik, O., and Goloub, P.:
Microscopic Observations of Core-Shell Particle Structure and Implications
for Atmospheric Aerosol Remote Sensing, J. Geophys. Res.-Atmos., 123, 13944–13962, https://doi.org/10.1029/2018jd028602, 2018.
Veghte, D. P., Bittner, D. R., and Freedman, M. A.: Cryo-Transmission Electron Microscopy Imaging of the Morphology of Submicrometer Aerosol
Containing Organic Acids and Ammonium Sulfate, Anal. Chem., 86, 2436–2442,
https://doi.org/10.1021/ac403279f, 2014.
Voorhees, P. W.: The Theory of Ostwald Ripening, J. Stat. Phys., 38, 231–252, https://doi.org/10.1007/Bf01017860, 1985.
Wang, N., Jing, B., Wang, P., Wang, Z., Li, J. R., Pang, S. F., Zhang, Y. H., and Ge, M. F.: Hygroscopicity and Compositional Evolution of Atmospheric
Aerosols Containing Water-Soluble Carboxylic Acid Salts and Ammonium Sulfate: Influence of Ammonium Depletion, Environ. Sci. Technol., 53, 6225–6234, https://doi.org/10.1021/acs.est.8b07052, 2019.
Wang, W. H., Shao, L. Y., Mazzoleni, C., Li, Y. W., Kotthaus, S., Grimmond,
S., Bhandari, J., Xing, J. P., Feng, X. L., Zhang, M. Y., and Shi, Z. B.:
Measurement report: Comparison of wintertime individual particles at ground
level and above the mixed layer in urban Beijing, Atmos. Chem. Phys., 21,
5301–5314, https://doi.org/10.5194/acp-21-5301-2021, 2021.
Wise, M. E., Martin, S. T., Russell, L. M., and Buseck, P. R.: Water Uptake
by NaCl Particles Prior to Deliquescence and the Phase Rule, Aerosol Sci. Tech., 42, 281–294, https://doi.org/10.1080/02786820802047115, 2008.
Xiong, C., Chen, X. Y., Ding, X. L., Kuang, B. Y., Pei, X. Y., Xu, Z. N., Yang, S. K., Hu, H., and Wang, Z. B.: Reconsideration of Surface Tension and
Phase State Effects on Cloud Condensation Nuclei Activity Based on the
Atomic Force Microscopy Measurement, Atmos. Chem. Phys., 22, 16123–16135,
https://doi.org/10.5194/acp-22-16123-2022, 2022.
Xiong, C., Kuang, B. Y., Zhang, F., Pei, X. Y., Xu, Z. N., and Wang, Z. B.: In-situ observation for RH-dependent mixing states of submicron particles containing organic surfactants and inorganic salts, Zenodo [data set], https://doi.org/10.5281/zenodo.8079001, 2023.
Xu, L., Fukushima, S., Sobanska, S., Murata, K., Naganuma, A., Liu, L., Wang, Y. Y., Niu, H. Y., Shi, Z. B., Kojima, T., Zhang, D. Z., and Li, W. J.: Tracing the evolution of morphology and mixing state of soot particles along with the movement of an Asian dust storm, Atmos. Chem. Phys., 20, 14321–14332, https://doi.org/10.5194/acp-20-14321-2020, 2020.
Xu, W. Q., Chen, C., Qiu, Y. M., Li, Y., Zhang, Z. Q., Karnezi, E., Pandis,
S. N., Xie, C. H., Li, Z. J., Sun, J. X., Ma, N., Xu, W. Y., Fu, P. Q., Wang, Z. F., Zhu, J., Worsnop, D. R., Ng, N. L., and Sun, Y. L.: Organic aerosol volatility and viscosity in the North China Plain: contrast between summer and winter, Atmos. Chem. Phys., 21, 5463–5476, https://doi.org/10.5194/acp-21-5463-2021, 2021.
Yang, H., Wang, N., Pang, S. F., Zheng, C. M., and Zhang, Y. H.: Chemical
reaction between sodium pyruvate and ammonium sulfate in aerosol particles
and resultant sodium sulfate efflorescence, Chemosphere, 215, 554–562,
https://doi.org/10.1016/j.chemosphere.2018.10.062, 2019.
You, Y. and Bertram, A. K.: Effects of Molecular Weight and Temperature on
Liquid-Liquid Phase Separation in Particles Containing Organic Species and
Inorganic Salts, Atmos. Chem. Phys., 15, 1351–1365, https://doi.org/10.5194/acp-15-1351-2015, 2015.
You, Y., Renbaum-Wolff, L., Carreras-Sospedra, M., Hanna, S. J., Hiranuma, N., Kamal, S., Smith, M. L., Zhang, X. L., Weber, R. J., Shilling, J. E.,
Dabdub, D., Martin, S. T., and Bertram, A. K.: Images Reveal that Atmospheric Particles can Undergo Liquid-Liquid Phase Separations, P. Natl. Acad. Sci. USA, 109, 13188–13193, https://doi.org/10.1073/pnas.1206414109, 2012.
You, Y., Renbaum-Wolff, L., and Bertram, A. K.: Liquid–liquid phase
separation in particles containing organics mixed with ammonium sulfate,
ammonium bisulfate, ammonium nitrate or sodium chloride, Atmos. Chem. Phys.,
13, 11723–11734, https://doi.org/10.5194/acp-13-11723-2013, 2013.
Závacká, K., Nedvela, V., Olbert, M., Tihlaříková, E., Vetráková, L., Yang, X., and Heger, D.: Temperature and Concentration Affect Particle Size Upon Sublimation Saline Ice: Implications for Sea Salt Aerosol Production in Polar Regions, Geophys. Res. Lett., 49, e2021GL097098, https://doi.org/10.1029/2021GL097098, 2022.
Zaveri, R. A., Easter, R. C., Fast, J. D., and Peters, L. K.: Model for
Simulating Aerosol Interactions and Chemistry (MOSAIC), J. Geophys. Res.-Atmos., 113, D13204, https://doi.org/10.1029/2007jd008782, 2008.
Zeng, G., Kelley, J., Kish, J. D., and Liu, Y.: Temperature-Dependent Deliquescent and Efflorescent Properties of Methanesulfonate Sodium Studied
by ATR-FTIR Spectroscopy, J. Phys. Chem. A, 118, 583–591, https://doi.org/10.1021/jp405896y, 2014.
Zhang, J., Yuan, Q., Liu, L., Wang, Y. Y., Zhang, Y. X., Xu, L., Pang, Y.,
Zhu, Y. H., Niu, H. Y., Shao, L. Y., Yang, S. S., Liu, H., Pan, X. L., Shi,
Z. B., Hu, M., Fu, P. Q., and Li, W. J.: Trans-Regional Transport of Haze
Particles From the North China Plain to Yangtze River Delta During Winter,
J. Geophys. Res.-Atmos., 126, e2020JD033778, https://doi.org/10.1029/2020JD033778, 2021.
Zhang, J., Wang, Y. Y., Teng, X. M., Liu, L., Xu, Y. S., Ren, L. H., Shi, Z.
B., Zhang, Y., Jiang, J. K., Liu, D. T., Hu, M., Shao, L. Y., Chen, J. M.,
Martin, S. T., Zhang, X. Y., and Li, W. J.: Liquid-Liquid Phase Separation
Reduces Radiative Absorption by Aged Black Carbon Aerosols, Commun. Earth
Environ., 3, 128, https://doi.org/10.1038/s43247-022-00462-1, 2022.
Zhang, Y., Chen, Y. Z., Lambe, A. T., Olson, N. E., Lei, Z. Y., Craig, R.
L., Zhang, Z. F., Gold, A., Onasch, T. B., Jayne, J. T., Worsnop, D. R.,
Gaston, C. J., Thornton, J. A., Vizuete, W., Ault, A. P., and Surratt, J.
D.: Effect of the Aerosol-Phase State on Secondary Organic Aerosol Formation
from the Reactive Uptake of Isoprene-Derived Epoxydiols (IEPDX), Environ.
Sci. Technol. Lett., 5, 167–174, https://doi.org/10.1021/acs.estlett.8b00044, 2018.
Zhang, Y. X., Zhang, Q., Yao, Z. L., and Li, H. Y.: Particle Size and Mixing
State of Freshly Emitted Black Carbon from Different Combustion Sources in
China, Environ. Sci. Technol., 54, 7766–7774, https://doi.org/10.1021/acs.est.9b07373, 2020.
Zhu, Y., Pang, S., and Zhang, Y.: Observations on the unique phase transitions of inorganics relevant due to gluconic acid in particles, Atmos.
Environ., 288, 119313, https://doi.org/10.1016/j.atmosenv.2022.119313, 2022.
Short summary
In hydration, an apparent water diffusion hindrance by an organic surfactant shell was confirmed, raising the inorganic deliquescence relative humidity (RH) to a nearly saturated condition. In dehydration, phase separations were observed for inorganic surfactant systems, showing a strong dependence on the organic molecular
oxygen-to-carbon ratio. Our results could improve fundamental knowledge about aerosol mixing states and decrease uncertainty in model estimations of global radiative effects.
In hydration, an apparent water diffusion hindrance by an organic surfactant shell was...
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