Water uptake of subpollen aerosol particles: hygroscopic growth, cloud condensation nuclei activation, and liquid–liquid phase separation

<p>Pollen grains emitted from vegetation can release subpollen particles (SPPs) that contribute to the fine fraction of atmospheric aerosols and may act as cloud condensation nuclei (CCN), ice nuclei (IN), or aeroallergens. Here, we investigate and characterize the hygroscopic growth and CCN a...

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Main Authors: E. F. Mikhailov, M. L. Pöhlker, K. Reinmuth-Selzle, S. S. Vlasenko, O. O. Krüger, J. Fröhlich-Nowoisky, C. Pöhlker, O. A. Ivanova, A. A. Kiselev, L. A. Kremper, U. Pöschl
Format: Article
Language:English
Published: Copernicus Publications 2021-05-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/21/6999/2021/acp-21-6999-2021.pdf
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spelling doaj-f91995c3ceaa42cf9563e91a1c7912ae2021-05-07T06:14:22ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242021-05-01216999702210.5194/acp-21-6999-2021Water uptake of subpollen aerosol particles: hygroscopic growth, cloud condensation nuclei activation, and liquid–liquid phase separationE. F. Mikhailov0E. F. Mikhailov1M. L. Pöhlker2K. Reinmuth-Selzle3S. S. Vlasenko4O. O. Krüger5J. Fröhlich-Nowoisky6C. Pöhlker7O. A. Ivanova8A. A. Kiselev9L. A. Kremper10U. Pöschl11Multiphase Chemistry and Biogeochemistry Departments, Max Planck Institute for Chemistry, 55020 Mainz, GermanyDepartment of Atmospheric Physics, Saint Petersburg State University, 7/9 Universitetskaya nab., St Petersburg, 199034, RussiaMultiphase Chemistry and Biogeochemistry Departments, Max Planck Institute for Chemistry, 55020 Mainz, GermanyMultiphase Chemistry and Biogeochemistry Departments, Max Planck Institute for Chemistry, 55020 Mainz, GermanyDepartment of Atmospheric Physics, Saint Petersburg State University, 7/9 Universitetskaya nab., St Petersburg, 199034, RussiaMultiphase Chemistry and Biogeochemistry Departments, Max Planck Institute for Chemistry, 55020 Mainz, GermanyMultiphase Chemistry and Biogeochemistry Departments, Max Planck Institute for Chemistry, 55020 Mainz, GermanyMultiphase Chemistry and Biogeochemistry Departments, Max Planck Institute for Chemistry, 55020 Mainz, GermanyDepartment of Atmospheric Physics, Saint Petersburg State University, 7/9 Universitetskaya nab., St Petersburg, 199034, RussiaAtmospheric Aerosol Research Department, Institute for Meteorology and Climate Research, Karlsruhe Institute of Technology (KIT), Hermann-von-Helmholtz Platz 1, 76344 Eggenstein-Leopoldshafen, GermanyMultiphase Chemistry and Biogeochemistry Departments, Max Planck Institute for Chemistry, 55020 Mainz, GermanyMultiphase Chemistry and Biogeochemistry Departments, Max Planck Institute for Chemistry, 55020 Mainz, Germany<p>Pollen grains emitted from vegetation can release subpollen particles (SPPs) that contribute to the fine fraction of atmospheric aerosols and may act as cloud condensation nuclei (CCN), ice nuclei (IN), or aeroallergens. Here, we investigate and characterize the hygroscopic growth and CCN activation of birch, pine, and rapeseed SPPs. A high-humidity tandem differential mobility analyzer (HHTDMA) was used to measure particle restructuring and water uptake over a wide range of relative humidity (RH) from 2 % to 99.5 %, and a continuous flow CCN counter was used for size-resolved measurements of CCN activation at supersaturations (<span class="inline-formula"><i>S</i></span>) in the range of 0.2 % to 1.2 %. For both subsaturated and supersaturated conditions, effective hygroscopicity parameters, <span class="inline-formula"><i>κ</i></span>, were obtained by Köhler model calculations. Gravimetric and chemical analyses, electron microscopy, and dynamic light scattering measurements were performed to characterize further properties of SPPs from aqueous pollen extracts such as chemical composition (starch, proteins, DNA, and inorganic ions) and the hydrodynamic size distribution of water-insoluble material. All investigated SPP samples exhibited a sharp increase of water uptake and <span class="inline-formula"><i>κ</i></span> above <span class="inline-formula">∼95</span> % RH, suggesting a liquid–liquid phase separation (LLPS). The HHTDMA measurements at RH <span class="inline-formula">&gt;95</span> % enable closure between the CCN activation at water vapor supersaturation and hygroscopic growth at subsaturated conditions, which is often not achieved when hygroscopicity tandem differential mobility analyzer (HTDMA) measurements are performed at lower RH where the water uptake and effective hygroscopicity may be limited by the effects of LLPS. Such effects may be important not only for closure between hygroscopic growth and CCN activation but also for the chemical reactivity, allergenic potential, and related health effects of SPPs.</p>https://acp.copernicus.org/articles/21/6999/2021/acp-21-6999-2021.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. F. Mikhailov
E. F. Mikhailov
M. L. Pöhlker
K. Reinmuth-Selzle
S. S. Vlasenko
O. O. Krüger
J. Fröhlich-Nowoisky
C. Pöhlker
O. A. Ivanova
A. A. Kiselev
L. A. Kremper
U. Pöschl
spellingShingle E. F. Mikhailov
E. F. Mikhailov
M. L. Pöhlker
K. Reinmuth-Selzle
S. S. Vlasenko
O. O. Krüger
J. Fröhlich-Nowoisky
C. Pöhlker
O. A. Ivanova
A. A. Kiselev
L. A. Kremper
U. Pöschl
Water uptake of subpollen aerosol particles: hygroscopic growth, cloud condensation nuclei activation, and liquid–liquid phase separation
Atmospheric Chemistry and Physics
author_facet E. F. Mikhailov
E. F. Mikhailov
M. L. Pöhlker
K. Reinmuth-Selzle
S. S. Vlasenko
O. O. Krüger
J. Fröhlich-Nowoisky
C. Pöhlker
O. A. Ivanova
A. A. Kiselev
L. A. Kremper
U. Pöschl
author_sort E. F. Mikhailov
title Water uptake of subpollen aerosol particles: hygroscopic growth, cloud condensation nuclei activation, and liquid–liquid phase separation
title_short Water uptake of subpollen aerosol particles: hygroscopic growth, cloud condensation nuclei activation, and liquid–liquid phase separation
title_full Water uptake of subpollen aerosol particles: hygroscopic growth, cloud condensation nuclei activation, and liquid–liquid phase separation
title_fullStr Water uptake of subpollen aerosol particles: hygroscopic growth, cloud condensation nuclei activation, and liquid–liquid phase separation
title_full_unstemmed Water uptake of subpollen aerosol particles: hygroscopic growth, cloud condensation nuclei activation, and liquid–liquid phase separation
title_sort water uptake of subpollen aerosol particles: hygroscopic growth, cloud condensation nuclei activation, and liquid–liquid phase separation
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2021-05-01
description <p>Pollen grains emitted from vegetation can release subpollen particles (SPPs) that contribute to the fine fraction of atmospheric aerosols and may act as cloud condensation nuclei (CCN), ice nuclei (IN), or aeroallergens. Here, we investigate and characterize the hygroscopic growth and CCN activation of birch, pine, and rapeseed SPPs. A high-humidity tandem differential mobility analyzer (HHTDMA) was used to measure particle restructuring and water uptake over a wide range of relative humidity (RH) from 2 % to 99.5 %, and a continuous flow CCN counter was used for size-resolved measurements of CCN activation at supersaturations (<span class="inline-formula"><i>S</i></span>) in the range of 0.2 % to 1.2 %. For both subsaturated and supersaturated conditions, effective hygroscopicity parameters, <span class="inline-formula"><i>κ</i></span>, were obtained by Köhler model calculations. Gravimetric and chemical analyses, electron microscopy, and dynamic light scattering measurements were performed to characterize further properties of SPPs from aqueous pollen extracts such as chemical composition (starch, proteins, DNA, and inorganic ions) and the hydrodynamic size distribution of water-insoluble material. All investigated SPP samples exhibited a sharp increase of water uptake and <span class="inline-formula"><i>κ</i></span> above <span class="inline-formula">∼95</span> % RH, suggesting a liquid–liquid phase separation (LLPS). The HHTDMA measurements at RH <span class="inline-formula">&gt;95</span> % enable closure between the CCN activation at water vapor supersaturation and hygroscopic growth at subsaturated conditions, which is often not achieved when hygroscopicity tandem differential mobility analyzer (HTDMA) measurements are performed at lower RH where the water uptake and effective hygroscopicity may be limited by the effects of LLPS. Such effects may be important not only for closure between hygroscopic growth and CCN activation but also for the chemical reactivity, allergenic potential, and related health effects of SPPs.</p>
url https://acp.copernicus.org/articles/21/6999/2021/acp-21-6999-2021.pdf
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