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Changes in nitrate accumulation mechanisms as PM2.5 levels increase on the North China Plain: A perspective from the dual isotopic compositions of nitrate
Nitrate (NO3−) has become recognized as the most important water-soluble ion in fine particulate (PM2.5), and has been proposed as a driving factor for regional haze formation. However, nitrate formation mechanisms are still poorly understood. In this study, PM2.5 samples were collected from Septemb...
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Published in: | Chemosphere (Oxford) 2021-01, Vol.263, p.127915, Article 127915 |
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description | Nitrate (NO3−) has become recognized as the most important water-soluble ion in fine particulate (PM2.5), and has been proposed as a driving factor for regional haze formation. However, nitrate formation mechanisms are still poorly understood. In this study, PM2.5 samples were collected from September 2017 to August 2018 in Shijiazhuang, a city located on the North China Plain, and NO3−concentration, δ18O-NO3− and δ15N-NO3− values in PM2.5 were analyzed. NO3− concentrations increased as PM2.5 levels increased during both polluted and non-polluted days over the entire year. δ18O-NO3− values during cold months (63.5–103‰) were higher than those during warm months (50.3–85.4‰), these results suggested that the nitrate formation pathways shifted from the NO2 + OH (POH) in warm months to the N2O5 + H2O (PN2O5) and NO3 + VOCs (PNO3) pathways in cold months. Especially during cold months, δ18O-NO3− values increased from 65.2–79.9‰ to 80.7–96.2‰ when PM2.5 increased from ∼25 to >100 μg/m3, but when PM2.5 > 100 μg/m3, there were relatively small variations in δ18O-NO3−. These results suggested that nitrate formation pathways changed from POH to PN2O5 and PNO3 pathways when PM2.5 < 100 μg/m3, but that PN2O5 and PNO3 dominated nitrate production when PM2.5 > 100 μg/m3. Higher δ15N-NO3− values in warm months (−11.8–13.8‰) than in cold months (−0.7–22.6‰) may be attributed to differences in NOx emission sources and nitrogen isotopic fractionation among NOx and NO3−. These results provide information on the dual isotopic compositions of nitrate to understand nitrate formation pathways under different PM2.5 levels.
•One-year values of δ18O-NO3− and δ15N-NO3− in PM2.5 were analyzed in Shijiazhuang.•Seasonal variations in δ18O-NO3− were affected by various nitrate formation pathways.•NO3− production shifted from POH to PN2O5+NO3 in cold months with increased PM2.5•Seasonal δ15N-NO3− was regulated by NOx sources and nitrogen isotopic fractionation. |
doi_str_mv | 10.1016/j.chemosphere.2020.127915 |
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•One-year values of δ18O-NO3− and δ15N-NO3− in PM2.5 were analyzed in Shijiazhuang.•Seasonal variations in δ18O-NO3− were affected by various nitrate formation pathways.•NO3− production shifted from POH to PN2O5+NO3 in cold months with increased PM2.5•Seasonal δ15N-NO3− was regulated by NOx sources and nitrogen isotopic fractionation.</description><identifier>ISSN: 0045-6535</identifier><identifier>DOI: 10.1016/j.chemosphere.2020.127915</identifier><language>eng</language><publisher>Elsevier Ltd</publisher><subject>Nitrate formation pathways ; PM2.5 ; Shijiazhuang ; δ15N-[formula omitted] ; δ18O-[formula omitted]</subject><ispartof>Chemosphere (Oxford), 2021-01, Vol.263, p.127915, Article 127915</ispartof><rights>2020 Elsevier Ltd</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c354t-3ab66d7543e16e0416dc43b1e8ba5d110bf72e610e4d0d3c21b164f11212a3bf3</citedby><cites>FETCH-LOGICAL-c354t-3ab66d7543e16e0416dc43b1e8ba5d110bf72e610e4d0d3c21b164f11212a3bf3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Luo, Li</creatorcontrib><creatorcontrib>Zhu, Ren-guo</creatorcontrib><creatorcontrib>Song, Cong-Bo</creatorcontrib><creatorcontrib>Peng, Jian-Fei</creatorcontrib><creatorcontrib>Guo, Wei</creatorcontrib><creatorcontrib>Liu, Yonghui</creatorcontrib><creatorcontrib>Zheng, Nengjian</creatorcontrib><creatorcontrib>Xiao, Hongwei</creatorcontrib><creatorcontrib>Xiao, Hua-Yun</creatorcontrib><title>Changes in nitrate accumulation mechanisms as PM2.5 levels increase on the North China Plain: A perspective from the dual isotopic compositions of nitrate</title><title>Chemosphere (Oxford)</title><description>Nitrate (NO3−) has become recognized as the most important water-soluble ion in fine particulate (PM2.5), and has been proposed as a driving factor for regional haze formation. However, nitrate formation mechanisms are still poorly understood. In this study, PM2.5 samples were collected from September 2017 to August 2018 in Shijiazhuang, a city located on the North China Plain, and NO3−concentration, δ18O-NO3− and δ15N-NO3− values in PM2.5 were analyzed. NO3− concentrations increased as PM2.5 levels increased during both polluted and non-polluted days over the entire year. δ18O-NO3− values during cold months (63.5–103‰) were higher than those during warm months (50.3–85.4‰), these results suggested that the nitrate formation pathways shifted from the NO2 + OH (POH) in warm months to the N2O5 + H2O (PN2O5) and NO3 + VOCs (PNO3) pathways in cold months. Especially during cold months, δ18O-NO3− values increased from 65.2–79.9‰ to 80.7–96.2‰ when PM2.5 increased from ∼25 to >100 μg/m3, but when PM2.5 > 100 μg/m3, there were relatively small variations in δ18O-NO3−. These results suggested that nitrate formation pathways changed from POH to PN2O5 and PNO3 pathways when PM2.5 < 100 μg/m3, but that PN2O5 and PNO3 dominated nitrate production when PM2.5 > 100 μg/m3. Higher δ15N-NO3− values in warm months (−11.8–13.8‰) than in cold months (−0.7–22.6‰) may be attributed to differences in NOx emission sources and nitrogen isotopic fractionation among NOx and NO3−. These results provide information on the dual isotopic compositions of nitrate to understand nitrate formation pathways under different PM2.5 levels.
•One-year values of δ18O-NO3− and δ15N-NO3− in PM2.5 were analyzed in Shijiazhuang.•Seasonal variations in δ18O-NO3− were affected by various nitrate formation pathways.•NO3− production shifted from POH to PN2O5+NO3 in cold months with increased PM2.5•Seasonal δ15N-NO3− was regulated by NOx sources and nitrogen isotopic fractionation.</description><subject>Nitrate formation pathways</subject><subject>PM2.5</subject><subject>Shijiazhuang</subject><subject>δ15N-[formula omitted]</subject><subject>δ18O-[formula omitted]</subject><issn>0045-6535</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNqNkMlOwzAQhn0AibK8w_AACV5il3KrIjapQA9wthxnQlwlcWS7lXgVnpaUgsSR00ij_5vlI-SS0ZxRpq42uW2x93FsMWDOKZ_6fL5g8ojMKC1kpqSQJ-Q0xg2lEyAXM_JZtmZ4xwhugMGlYBKCsXbbbzuTnB-gRzslXOwjmAjrJ55L6HCH3R6xAU1EmGKpRXj2IbVQtm4wsO6MG25gCSOGOKJNbofQBN9_J-ut6cBFn_zoLFjfjz66_boIvvm945wcN6aLePFTz8jb3e1r-ZCtXu4fy-Uqs0IWKROmUqqey0IgU0gLpmpbiIrhdWVkzRitmjlHxSgWNa2F5axiqmgY44wbUTXijCwOc23wMQZs9Bhcb8KHZlTvxeqN_iNW78Xqg9iJLQ_s5AN3DoOO1uFgsXZhelrX3v1jyheikIyp</recordid><startdate>202101</startdate><enddate>202101</enddate><creator>Luo, Li</creator><creator>Zhu, Ren-guo</creator><creator>Song, Cong-Bo</creator><creator>Peng, Jian-Fei</creator><creator>Guo, Wei</creator><creator>Liu, Yonghui</creator><creator>Zheng, Nengjian</creator><creator>Xiao, Hongwei</creator><creator>Xiao, Hua-Yun</creator><general>Elsevier Ltd</general><scope>AAYXX</scope><scope>CITATION</scope></search><sort><creationdate>202101</creationdate><title>Changes in nitrate accumulation mechanisms as PM2.5 levels increase on the North China Plain: A perspective from the dual isotopic compositions of nitrate</title><author>Luo, Li ; Zhu, Ren-guo ; Song, Cong-Bo ; Peng, Jian-Fei ; Guo, Wei ; Liu, Yonghui ; Zheng, Nengjian ; Xiao, Hongwei ; Xiao, Hua-Yun</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c354t-3ab66d7543e16e0416dc43b1e8ba5d110bf72e610e4d0d3c21b164f11212a3bf3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Nitrate formation pathways</topic><topic>PM2.5</topic><topic>Shijiazhuang</topic><topic>δ15N-[formula omitted]</topic><topic>δ18O-[formula omitted]</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Luo, Li</creatorcontrib><creatorcontrib>Zhu, Ren-guo</creatorcontrib><creatorcontrib>Song, Cong-Bo</creatorcontrib><creatorcontrib>Peng, Jian-Fei</creatorcontrib><creatorcontrib>Guo, Wei</creatorcontrib><creatorcontrib>Liu, Yonghui</creatorcontrib><creatorcontrib>Zheng, Nengjian</creatorcontrib><creatorcontrib>Xiao, Hongwei</creatorcontrib><creatorcontrib>Xiao, Hua-Yun</creatorcontrib><collection>CrossRef</collection><jtitle>Chemosphere (Oxford)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Luo, Li</au><au>Zhu, Ren-guo</au><au>Song, Cong-Bo</au><au>Peng, Jian-Fei</au><au>Guo, Wei</au><au>Liu, Yonghui</au><au>Zheng, Nengjian</au><au>Xiao, Hongwei</au><au>Xiao, Hua-Yun</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Changes in nitrate accumulation mechanisms as PM2.5 levels increase on the North China Plain: A perspective from the dual isotopic compositions of nitrate</atitle><jtitle>Chemosphere (Oxford)</jtitle><date>2021-01</date><risdate>2021</risdate><volume>263</volume><spage>127915</spage><pages>127915-</pages><artnum>127915</artnum><issn>0045-6535</issn><abstract>Nitrate (NO3−) has become recognized as the most important water-soluble ion in fine particulate (PM2.5), and has been proposed as a driving factor for regional haze formation. However, nitrate formation mechanisms are still poorly understood. In this study, PM2.5 samples were collected from September 2017 to August 2018 in Shijiazhuang, a city located on the North China Plain, and NO3−concentration, δ18O-NO3− and δ15N-NO3− values in PM2.5 were analyzed. NO3− concentrations increased as PM2.5 levels increased during both polluted and non-polluted days over the entire year. δ18O-NO3− values during cold months (63.5–103‰) were higher than those during warm months (50.3–85.4‰), these results suggested that the nitrate formation pathways shifted from the NO2 + OH (POH) in warm months to the N2O5 + H2O (PN2O5) and NO3 + VOCs (PNO3) pathways in cold months. Especially during cold months, δ18O-NO3− values increased from 65.2–79.9‰ to 80.7–96.2‰ when PM2.5 increased from ∼25 to >100 μg/m3, but when PM2.5 > 100 μg/m3, there were relatively small variations in δ18O-NO3−. These results suggested that nitrate formation pathways changed from POH to PN2O5 and PNO3 pathways when PM2.5 < 100 μg/m3, but that PN2O5 and PNO3 dominated nitrate production when PM2.5 > 100 μg/m3. Higher δ15N-NO3− values in warm months (−11.8–13.8‰) than in cold months (−0.7–22.6‰) may be attributed to differences in NOx emission sources and nitrogen isotopic fractionation among NOx and NO3−. These results provide information on the dual isotopic compositions of nitrate to understand nitrate formation pathways under different PM2.5 levels.
•One-year values of δ18O-NO3− and δ15N-NO3− in PM2.5 were analyzed in Shijiazhuang.•Seasonal variations in δ18O-NO3− were affected by various nitrate formation pathways.•NO3− production shifted from POH to PN2O5+NO3 in cold months with increased PM2.5•Seasonal δ15N-NO3− was regulated by NOx sources and nitrogen isotopic fractionation.</abstract><pub>Elsevier Ltd</pub><doi>10.1016/j.chemosphere.2020.127915</doi></addata></record> |
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title | Changes in nitrate accumulation mechanisms as PM2.5 levels increase on the North China Plain: A perspective from the dual isotopic compositions of nitrate |
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