Investigating the hygroscopicities of calcium and magnesium salt particles aged with SO2 using surface plasmon resonance microscopy

The hygroscopicities of calcium and magnesium salts strongly affect the environment and climate, but the aging products of these salts at high relative humidities (RHs) are still poorly understood. In this study, surface plasmon resonance microscopy (SPRM) was used to determine the hygroscopic growt...

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Veröffentlicht in:The Science of the total environment 2023-04, Vol.867, p.161588-161588, Article 161588
Hauptverfasser: Yang, Bo, Xie, Zhibo, Liu, Jianguo, Gui, Huaqiao, Zhang, Jiaoshi, Wei, Xiuli, Wang, Jie, Fan, Zetao, Zhang, Douguo
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container_title The Science of the total environment
container_volume 867
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Xie, Zhibo
Liu, Jianguo
Gui, Huaqiao
Zhang, Jiaoshi
Wei, Xiuli
Wang, Jie
Fan, Zetao
Zhang, Douguo
description The hygroscopicities of calcium and magnesium salts strongly affect the environment and climate, but the aging products of these salts at high relative humidities (RHs) are still poorly understood. In this study, surface plasmon resonance microscopy (SPRM) was used to determine the hygroscopic growth factors (GFs) of Ca(NO3)2 and Mg(NO3)2 separately or mixed with galactose at different mass ratios at different RHs before and after aging. For all particles, the measured GFs showed no indication of deliquescence across the range of RHs tested, and overall hygroscopicity was clearly lower after than before aging. The Ca(NO3)2 and Mg(NO3)2 GFs at 90 % RH were 1.80 and 1.66, respectively, before aging and 1.33 and 1.42, respectively, after 4 h aging, meaning aging decreased the GFs by 26.11 % and 14.46 %, respectively. Aging decreased the hygroscopicity because insoluble or sparingly soluble substances (CaSO3, CaSO4, MgSO3) formed and strongly changed the overall hygroscopicity. For bicomponent aerosols with different mass ratios, the GFs (calculated using the Zdanovskii-Stokes-Robinson method) of the other components except galactose at 90 % RH after 1 h aging were all lower, respectively, than the measured GFs of pure Ca(NO3)2 and Mg(NO3)2 after aging for 1 h, especially with the mass ratio of 1:2, their GFs have decreased by 14.63 % and 7.50 %, respectively. Subsequently, Ion chromatograms indicated that the peak area ratio of SO42− to NO3− ratios were higher for the aged bicomponent particles than aged single-component particles, possibly because adding galactose improved the gas–liquid state stability during drying after the aging process and therefore promoted nitrate consumption and sulfate formation. The results indicated that organic components may play important roles in heterogeneous reactions between trace gases and multicomponent aerosols and should be considered in evaluating the impacts on submicron aerosol composition of high atmospheric SO2 concentrations at high humidities. [Display omitted] •Nanoparticles hygroscopicity is analyzed by surface plasmon resonance microscopy.•Reaction products of SO2 uptake by mixed nitrate aerosols are poorly understood.•The growth factors of nitrate aerosols were determined before and after aging.•The addition of organic components can promote aging of multicomponent aerosols.
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In this study, surface plasmon resonance microscopy (SPRM) was used to determine the hygroscopic growth factors (GFs) of Ca(NO3)2 and Mg(NO3)2 separately or mixed with galactose at different mass ratios at different RHs before and after aging. For all particles, the measured GFs showed no indication of deliquescence across the range of RHs tested, and overall hygroscopicity was clearly lower after than before aging. The Ca(NO3)2 and Mg(NO3)2 GFs at 90 % RH were 1.80 and 1.66, respectively, before aging and 1.33 and 1.42, respectively, after 4 h aging, meaning aging decreased the GFs by 26.11 % and 14.46 %, respectively. Aging decreased the hygroscopicity because insoluble or sparingly soluble substances (CaSO3, CaSO4, MgSO3) formed and strongly changed the overall hygroscopicity. For bicomponent aerosols with different mass ratios, the GFs (calculated using the Zdanovskii-Stokes-Robinson method) of the other components except galactose at 90 % RH after 1 h aging were all lower, respectively, than the measured GFs of pure Ca(NO3)2 and Mg(NO3)2 after aging for 1 h, especially with the mass ratio of 1:2, their GFs have decreased by 14.63 % and 7.50 %, respectively. Subsequently, Ion chromatograms indicated that the peak area ratio of SO42− to NO3− ratios were higher for the aged bicomponent particles than aged single-component particles, possibly because adding galactose improved the gas–liquid state stability during drying after the aging process and therefore promoted nitrate consumption and sulfate formation. The results indicated that organic components may play important roles in heterogeneous reactions between trace gases and multicomponent aerosols and should be considered in evaluating the impacts on submicron aerosol composition of high atmospheric SO2 concentrations at high humidities. [Display omitted] •Nanoparticles hygroscopicity is analyzed by surface plasmon resonance microscopy.•Reaction products of SO2 uptake by mixed nitrate aerosols are poorly understood.•The growth factors of nitrate aerosols were determined before and after aging.•The addition of organic components can promote aging of multicomponent aerosols.</description><identifier>ISSN: 0048-9697</identifier><identifier>EISSN: 1879-1026</identifier><identifier>DOI: 10.1016/j.scitotenv.2023.161588</identifier><language>eng</language><publisher>Elsevier B.V</publisher><subject>Aging ; Calcium and magnesium salts ; Hygroscopic growth ; Surface plasmon resonance ; Ultrafine particle</subject><ispartof>The Science of the total environment, 2023-04, Vol.867, p.161588-161588, Article 161588</ispartof><rights>2023 Elsevier B.V.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c348t-db8a0a9099b4ba815dfe72ae4992ca6a0e28694731824fd7360be98ea05dbe163</citedby><cites>FETCH-LOGICAL-c348t-db8a0a9099b4ba815dfe72ae4992ca6a0e28694731824fd7360be98ea05dbe163</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://www.sciencedirect.com/science/article/pii/S0048969723002036$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,776,780,3536,27903,27904,65309</link.rule.ids></links><search><creatorcontrib>Yang, Bo</creatorcontrib><creatorcontrib>Xie, Zhibo</creatorcontrib><creatorcontrib>Liu, Jianguo</creatorcontrib><creatorcontrib>Gui, Huaqiao</creatorcontrib><creatorcontrib>Zhang, Jiaoshi</creatorcontrib><creatorcontrib>Wei, Xiuli</creatorcontrib><creatorcontrib>Wang, Jie</creatorcontrib><creatorcontrib>Fan, Zetao</creatorcontrib><creatorcontrib>Zhang, Douguo</creatorcontrib><title>Investigating the hygroscopicities of calcium and magnesium salt particles aged with SO2 using surface plasmon resonance microscopy</title><title>The Science of the total environment</title><description>The hygroscopicities of calcium and magnesium salts strongly affect the environment and climate, but the aging products of these salts at high relative humidities (RHs) are still poorly understood. In this study, surface plasmon resonance microscopy (SPRM) was used to determine the hygroscopic growth factors (GFs) of Ca(NO3)2 and Mg(NO3)2 separately or mixed with galactose at different mass ratios at different RHs before and after aging. For all particles, the measured GFs showed no indication of deliquescence across the range of RHs tested, and overall hygroscopicity was clearly lower after than before aging. The Ca(NO3)2 and Mg(NO3)2 GFs at 90 % RH were 1.80 and 1.66, respectively, before aging and 1.33 and 1.42, respectively, after 4 h aging, meaning aging decreased the GFs by 26.11 % and 14.46 %, respectively. Aging decreased the hygroscopicity because insoluble or sparingly soluble substances (CaSO3, CaSO4, MgSO3) formed and strongly changed the overall hygroscopicity. For bicomponent aerosols with different mass ratios, the GFs (calculated using the Zdanovskii-Stokes-Robinson method) of the other components except galactose at 90 % RH after 1 h aging were all lower, respectively, than the measured GFs of pure Ca(NO3)2 and Mg(NO3)2 after aging for 1 h, especially with the mass ratio of 1:2, their GFs have decreased by 14.63 % and 7.50 %, respectively. Subsequently, Ion chromatograms indicated that the peak area ratio of SO42− to NO3− ratios were higher for the aged bicomponent particles than aged single-component particles, possibly because adding galactose improved the gas–liquid state stability during drying after the aging process and therefore promoted nitrate consumption and sulfate formation. The results indicated that organic components may play important roles in heterogeneous reactions between trace gases and multicomponent aerosols and should be considered in evaluating the impacts on submicron aerosol composition of high atmospheric SO2 concentrations at high humidities. [Display omitted] •Nanoparticles hygroscopicity is analyzed by surface plasmon resonance microscopy.•Reaction products of SO2 uptake by mixed nitrate aerosols are poorly understood.•The growth factors of nitrate aerosols were determined before and after aging.•The addition of organic components can promote aging of multicomponent aerosols.</description><subject>Aging</subject><subject>Calcium and magnesium salts</subject><subject>Hygroscopic growth</subject><subject>Surface plasmon resonance</subject><subject>Ultrafine particle</subject><issn>0048-9697</issn><issn>1879-1026</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNqFUMuO1DAQtBBIDAvfgI9cMthOxrGPqxWPlVbaA3C2Ok4n41FiB9sZNGd-HEdBXOlLq1tV1V1FyHvOjpxx-fFyTNblkNFfj4KJ-sglPyn1ghy4anXFmZAvyYGxRlVa6vY1eZPShZVqFT-Q34_-iim7EbLzI81npOfbGEOyYXFF12GiYaAWJuvWmYLv6Qyjx7RNCaZMF4jZ2angYMSe_nL5TL89C7qmTTCtcQCLdJkgzcHTiCl48GUzO7ufub0lrwaYEr772-_Ij8-fvj98rZ6evzw-3D9Vtm5UrvpOAQPNtO6aDhQ_9QO2ArDRWliQwFAoqZu25ko0Q9_WknWoFQI79R1yWd-RD7vuEsPPtbg2s0sWpwk8hjUZ0UrJpKxrXqDtDt1-TBEHs0Q3Q7wZzswWu7mYf7GbLXazx16Y9zsTi5Orw7jhsBjuXUSbTR_cfzX-AANdk-U</recordid><startdate>20230401</startdate><enddate>20230401</enddate><creator>Yang, Bo</creator><creator>Xie, Zhibo</creator><creator>Liu, Jianguo</creator><creator>Gui, Huaqiao</creator><creator>Zhang, Jiaoshi</creator><creator>Wei, Xiuli</creator><creator>Wang, Jie</creator><creator>Fan, Zetao</creator><creator>Zhang, Douguo</creator><general>Elsevier B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7X8</scope></search><sort><creationdate>20230401</creationdate><title>Investigating the hygroscopicities of calcium and magnesium salt particles aged with SO2 using surface plasmon resonance microscopy</title><author>Yang, Bo ; Xie, Zhibo ; Liu, Jianguo ; Gui, Huaqiao ; Zhang, Jiaoshi ; Wei, Xiuli ; Wang, Jie ; Fan, Zetao ; Zhang, Douguo</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c348t-db8a0a9099b4ba815dfe72ae4992ca6a0e28694731824fd7360be98ea05dbe163</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Aging</topic><topic>Calcium and magnesium salts</topic><topic>Hygroscopic growth</topic><topic>Surface plasmon resonance</topic><topic>Ultrafine particle</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Yang, Bo</creatorcontrib><creatorcontrib>Xie, Zhibo</creatorcontrib><creatorcontrib>Liu, Jianguo</creatorcontrib><creatorcontrib>Gui, Huaqiao</creatorcontrib><creatorcontrib>Zhang, Jiaoshi</creatorcontrib><creatorcontrib>Wei, Xiuli</creatorcontrib><creatorcontrib>Wang, Jie</creatorcontrib><creatorcontrib>Fan, Zetao</creatorcontrib><creatorcontrib>Zhang, Douguo</creatorcontrib><collection>CrossRef</collection><collection>MEDLINE - Academic</collection><jtitle>The Science of the total environment</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Yang, Bo</au><au>Xie, Zhibo</au><au>Liu, Jianguo</au><au>Gui, Huaqiao</au><au>Zhang, Jiaoshi</au><au>Wei, Xiuli</au><au>Wang, Jie</au><au>Fan, Zetao</au><au>Zhang, Douguo</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Investigating the hygroscopicities of calcium and magnesium salt particles aged with SO2 using surface plasmon resonance microscopy</atitle><jtitle>The Science of the total environment</jtitle><date>2023-04-01</date><risdate>2023</risdate><volume>867</volume><spage>161588</spage><epage>161588</epage><pages>161588-161588</pages><artnum>161588</artnum><issn>0048-9697</issn><eissn>1879-1026</eissn><abstract>The hygroscopicities of calcium and magnesium salts strongly affect the environment and climate, but the aging products of these salts at high relative humidities (RHs) are still poorly understood. In this study, surface plasmon resonance microscopy (SPRM) was used to determine the hygroscopic growth factors (GFs) of Ca(NO3)2 and Mg(NO3)2 separately or mixed with galactose at different mass ratios at different RHs before and after aging. For all particles, the measured GFs showed no indication of deliquescence across the range of RHs tested, and overall hygroscopicity was clearly lower after than before aging. The Ca(NO3)2 and Mg(NO3)2 GFs at 90 % RH were 1.80 and 1.66, respectively, before aging and 1.33 and 1.42, respectively, after 4 h aging, meaning aging decreased the GFs by 26.11 % and 14.46 %, respectively. Aging decreased the hygroscopicity because insoluble or sparingly soluble substances (CaSO3, CaSO4, MgSO3) formed and strongly changed the overall hygroscopicity. For bicomponent aerosols with different mass ratios, the GFs (calculated using the Zdanovskii-Stokes-Robinson method) of the other components except galactose at 90 % RH after 1 h aging were all lower, respectively, than the measured GFs of pure Ca(NO3)2 and Mg(NO3)2 after aging for 1 h, especially with the mass ratio of 1:2, their GFs have decreased by 14.63 % and 7.50 %, respectively. Subsequently, Ion chromatograms indicated that the peak area ratio of SO42− to NO3− ratios were higher for the aged bicomponent particles than aged single-component particles, possibly because adding galactose improved the gas–liquid state stability during drying after the aging process and therefore promoted nitrate consumption and sulfate formation. The results indicated that organic components may play important roles in heterogeneous reactions between trace gases and multicomponent aerosols and should be considered in evaluating the impacts on submicron aerosol composition of high atmospheric SO2 concentrations at high humidities. [Display omitted] •Nanoparticles hygroscopicity is analyzed by surface plasmon resonance microscopy.•Reaction products of SO2 uptake by mixed nitrate aerosols are poorly understood.•The growth factors of nitrate aerosols were determined before and after aging.•The addition of organic components can promote aging of multicomponent aerosols.</abstract><pub>Elsevier B.V</pub><doi>10.1016/j.scitotenv.2023.161588</doi><tpages>1</tpages></addata></record>
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subjects Aging
Calcium and magnesium salts
Hygroscopic growth
Surface plasmon resonance
Ultrafine particle
title Investigating the hygroscopicities of calcium and magnesium salt particles aged with SO2 using surface plasmon resonance microscopy
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