Cloud Condensation Nuclei Activity and Hygroscopicity of Fresh and Aged Biomass Burning Particles
Abstract Biomass burning particles are one of the largest aerosol sources worldwide and contribute a significant fraction of the global cloud condensation nuclei (CCN) burden. Chemical aging experiments of sawgrass burning particles took place in a smog chamber by turning on the UV light after HONO...
Ausführliche Beschreibung
Autor*in: |
Li, Yanwei [verfasserIn] |
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Format: |
Artikel |
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Sprache: |
Englisch |
Erschienen: |
2018 |
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Schlagwörter: |
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Anmerkung: |
© The Author(s) 2018 |
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Übergeordnetes Werk: |
Enthalten in: Pure and applied geophysics - Springer International Publishing, 1964, 176(2018), 1 vom: 26. Juni, Seite 345-356 |
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Übergeordnetes Werk: |
volume:176 ; year:2018 ; number:1 ; day:26 ; month:06 ; pages:345-356 |
Links: |
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DOI / URN: |
10.1007/s00024-018-1903-0 |
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Katalog-ID: |
OLC2069510816 |
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520 | |a Abstract Biomass burning particles are one of the largest aerosol sources worldwide and contribute a significant fraction of the global cloud condensation nuclei (CCN) burden. Chemical aging experiments of sawgrass burning particles took place in a smog chamber by turning on the UV light after HONO or $ H_{2} $$ O_{2} $ injection. The CCN activity and corresponding hygroscopicity of fresh and aged particles were measured. Most of the fresh particles can serve as reasonable CCN, and the average activation diameters at 0.2% supersaturation were 114–125 nm in the experiments. The aging process caused that the mass fraction of organic aerosols decrease and condensed phase nitrate $ NO_{3} $− increase, and also the average atomic oxygen to carbon (O:C) ratios increase, which were the main reasons that the aged particles were more CCN active and hygroscopic. The average activation diameters decreased by 8–15% at 0.2% supersaturation after aging, and hygroscopic parameter κ increased by 30–42%. The chemical aging productions were a little different in experiments, but the CCN property and hygroscopicity change trends were quite similar. | ||
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10.1007/s00024-018-1903-0 doi (DE-627)OLC2069510816 (DE-He213)s00024-018-1903-0-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Li, Yanwei verfasserin (orcid)0000-0002-5375-1751 aut Cloud Condensation Nuclei Activity and Hygroscopicity of Fresh and Aged Biomass Burning Particles 2018 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2018 Abstract Biomass burning particles are one of the largest aerosol sources worldwide and contribute a significant fraction of the global cloud condensation nuclei (CCN) burden. Chemical aging experiments of sawgrass burning particles took place in a smog chamber by turning on the UV light after HONO or $ H_{2} $$ O_{2} $ injection. The CCN activity and corresponding hygroscopicity of fresh and aged particles were measured. Most of the fresh particles can serve as reasonable CCN, and the average activation diameters at 0.2% supersaturation were 114–125 nm in the experiments. The aging process caused that the mass fraction of organic aerosols decrease and condensed phase nitrate $ NO_{3} $− increase, and also the average atomic oxygen to carbon (O:C) ratios increase, which were the main reasons that the aged particles were more CCN active and hygroscopic. The average activation diameters decreased by 8–15% at 0.2% supersaturation after aging, and hygroscopic parameter κ increased by 30–42%. The chemical aging productions were a little different in experiments, but the CCN property and hygroscopicity change trends were quite similar. Biomass burning particles hygroscopic properties CCN chemical aging Enthalten in Pure and applied geophysics Springer International Publishing, 1964 176(2018), 1 vom: 26. Juni, Seite 345-356 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:176 year:2018 number:1 day:26 month:06 pages:345-356 https://doi.org/10.1007/s00024-018-1903-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 AR 176 2018 1 26 06 345-356 |
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10.1007/s00024-018-1903-0 doi (DE-627)OLC2069510816 (DE-He213)s00024-018-1903-0-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Li, Yanwei verfasserin (orcid)0000-0002-5375-1751 aut Cloud Condensation Nuclei Activity and Hygroscopicity of Fresh and Aged Biomass Burning Particles 2018 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2018 Abstract Biomass burning particles are one of the largest aerosol sources worldwide and contribute a significant fraction of the global cloud condensation nuclei (CCN) burden. Chemical aging experiments of sawgrass burning particles took place in a smog chamber by turning on the UV light after HONO or $ H_{2} $$ O_{2} $ injection. The CCN activity and corresponding hygroscopicity of fresh and aged particles were measured. Most of the fresh particles can serve as reasonable CCN, and the average activation diameters at 0.2% supersaturation were 114–125 nm in the experiments. The aging process caused that the mass fraction of organic aerosols decrease and condensed phase nitrate $ NO_{3} $− increase, and also the average atomic oxygen to carbon (O:C) ratios increase, which were the main reasons that the aged particles were more CCN active and hygroscopic. The average activation diameters decreased by 8–15% at 0.2% supersaturation after aging, and hygroscopic parameter κ increased by 30–42%. The chemical aging productions were a little different in experiments, but the CCN property and hygroscopicity change trends were quite similar. Biomass burning particles hygroscopic properties CCN chemical aging Enthalten in Pure and applied geophysics Springer International Publishing, 1964 176(2018), 1 vom: 26. Juni, Seite 345-356 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:176 year:2018 number:1 day:26 month:06 pages:345-356 https://doi.org/10.1007/s00024-018-1903-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 AR 176 2018 1 26 06 345-356 |
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10.1007/s00024-018-1903-0 doi (DE-627)OLC2069510816 (DE-He213)s00024-018-1903-0-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Li, Yanwei verfasserin (orcid)0000-0002-5375-1751 aut Cloud Condensation Nuclei Activity and Hygroscopicity of Fresh and Aged Biomass Burning Particles 2018 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2018 Abstract Biomass burning particles are one of the largest aerosol sources worldwide and contribute a significant fraction of the global cloud condensation nuclei (CCN) burden. Chemical aging experiments of sawgrass burning particles took place in a smog chamber by turning on the UV light after HONO or $ H_{2} $$ O_{2} $ injection. The CCN activity and corresponding hygroscopicity of fresh and aged particles were measured. Most of the fresh particles can serve as reasonable CCN, and the average activation diameters at 0.2% supersaturation were 114–125 nm in the experiments. The aging process caused that the mass fraction of organic aerosols decrease and condensed phase nitrate $ NO_{3} $− increase, and also the average atomic oxygen to carbon (O:C) ratios increase, which were the main reasons that the aged particles were more CCN active and hygroscopic. The average activation diameters decreased by 8–15% at 0.2% supersaturation after aging, and hygroscopic parameter κ increased by 30–42%. The chemical aging productions were a little different in experiments, but the CCN property and hygroscopicity change trends were quite similar. Biomass burning particles hygroscopic properties CCN chemical aging Enthalten in Pure and applied geophysics Springer International Publishing, 1964 176(2018), 1 vom: 26. Juni, Seite 345-356 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:176 year:2018 number:1 day:26 month:06 pages:345-356 https://doi.org/10.1007/s00024-018-1903-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 AR 176 2018 1 26 06 345-356 |
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10.1007/s00024-018-1903-0 doi (DE-627)OLC2069510816 (DE-He213)s00024-018-1903-0-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Li, Yanwei verfasserin (orcid)0000-0002-5375-1751 aut Cloud Condensation Nuclei Activity and Hygroscopicity of Fresh and Aged Biomass Burning Particles 2018 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2018 Abstract Biomass burning particles are one of the largest aerosol sources worldwide and contribute a significant fraction of the global cloud condensation nuclei (CCN) burden. Chemical aging experiments of sawgrass burning particles took place in a smog chamber by turning on the UV light after HONO or $ H_{2} $$ O_{2} $ injection. The CCN activity and corresponding hygroscopicity of fresh and aged particles were measured. Most of the fresh particles can serve as reasonable CCN, and the average activation diameters at 0.2% supersaturation were 114–125 nm in the experiments. The aging process caused that the mass fraction of organic aerosols decrease and condensed phase nitrate $ NO_{3} $− increase, and also the average atomic oxygen to carbon (O:C) ratios increase, which were the main reasons that the aged particles were more CCN active and hygroscopic. The average activation diameters decreased by 8–15% at 0.2% supersaturation after aging, and hygroscopic parameter κ increased by 30–42%. The chemical aging productions were a little different in experiments, but the CCN property and hygroscopicity change trends were quite similar. Biomass burning particles hygroscopic properties CCN chemical aging Enthalten in Pure and applied geophysics Springer International Publishing, 1964 176(2018), 1 vom: 26. Juni, Seite 345-356 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:176 year:2018 number:1 day:26 month:06 pages:345-356 https://doi.org/10.1007/s00024-018-1903-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 AR 176 2018 1 26 06 345-356 |
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10.1007/s00024-018-1903-0 doi (DE-627)OLC2069510816 (DE-He213)s00024-018-1903-0-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 16,13 ssgn Li, Yanwei verfasserin (orcid)0000-0002-5375-1751 aut Cloud Condensation Nuclei Activity and Hygroscopicity of Fresh and Aged Biomass Burning Particles 2018 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s) 2018 Abstract Biomass burning particles are one of the largest aerosol sources worldwide and contribute a significant fraction of the global cloud condensation nuclei (CCN) burden. Chemical aging experiments of sawgrass burning particles took place in a smog chamber by turning on the UV light after HONO or $ H_{2} $$ O_{2} $ injection. The CCN activity and corresponding hygroscopicity of fresh and aged particles were measured. Most of the fresh particles can serve as reasonable CCN, and the average activation diameters at 0.2% supersaturation were 114–125 nm in the experiments. The aging process caused that the mass fraction of organic aerosols decrease and condensed phase nitrate $ NO_{3} $− increase, and also the average atomic oxygen to carbon (O:C) ratios increase, which were the main reasons that the aged particles were more CCN active and hygroscopic. The average activation diameters decreased by 8–15% at 0.2% supersaturation after aging, and hygroscopic parameter κ increased by 30–42%. The chemical aging productions were a little different in experiments, but the CCN property and hygroscopicity change trends were quite similar. Biomass burning particles hygroscopic properties CCN chemical aging Enthalten in Pure and applied geophysics Springer International Publishing, 1964 176(2018), 1 vom: 26. Juni, Seite 345-356 (DE-627)129538353 (DE-600)216719-0 (DE-576)014971038 0033-4553 nnns volume:176 year:2018 number:1 day:26 month:06 pages:345-356 https://doi.org/10.1007/s00024-018-1903-0 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 AR 176 2018 1 26 06 345-356 |
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cloud condensation nuclei activity and hygroscopicity of fresh and aged biomass burning particles |
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Cloud Condensation Nuclei Activity and Hygroscopicity of Fresh and Aged Biomass Burning Particles |
abstract |
Abstract Biomass burning particles are one of the largest aerosol sources worldwide and contribute a significant fraction of the global cloud condensation nuclei (CCN) burden. Chemical aging experiments of sawgrass burning particles took place in a smog chamber by turning on the UV light after HONO or $ H_{2} $$ O_{2} $ injection. The CCN activity and corresponding hygroscopicity of fresh and aged particles were measured. Most of the fresh particles can serve as reasonable CCN, and the average activation diameters at 0.2% supersaturation were 114–125 nm in the experiments. The aging process caused that the mass fraction of organic aerosols decrease and condensed phase nitrate $ NO_{3} $− increase, and also the average atomic oxygen to carbon (O:C) ratios increase, which were the main reasons that the aged particles were more CCN active and hygroscopic. The average activation diameters decreased by 8–15% at 0.2% supersaturation after aging, and hygroscopic parameter κ increased by 30–42%. The chemical aging productions were a little different in experiments, but the CCN property and hygroscopicity change trends were quite similar. © The Author(s) 2018 |
abstractGer |
Abstract Biomass burning particles are one of the largest aerosol sources worldwide and contribute a significant fraction of the global cloud condensation nuclei (CCN) burden. Chemical aging experiments of sawgrass burning particles took place in a smog chamber by turning on the UV light after HONO or $ H_{2} $$ O_{2} $ injection. The CCN activity and corresponding hygroscopicity of fresh and aged particles were measured. Most of the fresh particles can serve as reasonable CCN, and the average activation diameters at 0.2% supersaturation were 114–125 nm in the experiments. The aging process caused that the mass fraction of organic aerosols decrease and condensed phase nitrate $ NO_{3} $− increase, and also the average atomic oxygen to carbon (O:C) ratios increase, which were the main reasons that the aged particles were more CCN active and hygroscopic. The average activation diameters decreased by 8–15% at 0.2% supersaturation after aging, and hygroscopic parameter κ increased by 30–42%. The chemical aging productions were a little different in experiments, but the CCN property and hygroscopicity change trends were quite similar. © The Author(s) 2018 |
abstract_unstemmed |
Abstract Biomass burning particles are one of the largest aerosol sources worldwide and contribute a significant fraction of the global cloud condensation nuclei (CCN) burden. Chemical aging experiments of sawgrass burning particles took place in a smog chamber by turning on the UV light after HONO or $ H_{2} $$ O_{2} $ injection. The CCN activity and corresponding hygroscopicity of fresh and aged particles were measured. Most of the fresh particles can serve as reasonable CCN, and the average activation diameters at 0.2% supersaturation were 114–125 nm in the experiments. The aging process caused that the mass fraction of organic aerosols decrease and condensed phase nitrate $ NO_{3} $− increase, and also the average atomic oxygen to carbon (O:C) ratios increase, which were the main reasons that the aged particles were more CCN active and hygroscopic. The average activation diameters decreased by 8–15% at 0.2% supersaturation after aging, and hygroscopic parameter κ increased by 30–42%. The chemical aging productions were a little different in experiments, but the CCN property and hygroscopicity change trends were quite similar. © The Author(s) 2018 |
collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-GEO SSG-OLC-PHA SSG-OLC-DE-84 SSG-OPC-GGO SSG-OPC-GEO GBV_ILN_70 GBV_ILN_267 GBV_ILN_601 |
container_issue |
1 |
title_short |
Cloud Condensation Nuclei Activity and Hygroscopicity of Fresh and Aged Biomass Burning Particles |
url |
https://doi.org/10.1007/s00024-018-1903-0 |
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doi_str |
10.1007/s00024-018-1903-0 |
up_date |
2024-07-03T22:28:32.047Z |
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