Yan-Li Wang, Xue‐Yan Liu, Wei Song, Wen Yang, B. Han, Xiaoyan Dou, Xu-Dong Zhao, Zhaoliang Song, Cong‐Qiang Liu, Z. Bai
{"title":"基于体δ15N特征和贝叶斯同位素混合模型的PM2.5中氮源确定","authors":"Yan-Li Wang, Xue‐Yan Liu, Wei Song, Wen Yang, B. Han, Xiaoyan Dou, Xu-Dong Zhao, Zhaoliang Song, Cong‐Qiang Liu, Z. Bai","doi":"10.1080/16000889.2017.1299672","DOIUrl":null,"url":null,"abstract":"Abstract Nitrogen isotope (δ15N) has been employed to differentiate major sources of atmospheric N. However, it remains a challenge to quantify contributions of multiple sources based on δ15N values of the N mixture in atmospheric samples. This study measured δ15N of bulk N in PM2.5 at an urban site of Beijing during a severe haze episode of 22–30 January 2013 and a background site of Qinghai, north-western China from 6 September to 15 October 2013, then applied a Bayesian isotope mixing model (SIAR, Stable Isotope Analysis in R) to analyse the N sources. At Beijing site, δ15N values of PM2.5 (−4.1‰ to +13.5‰, +2.8 ± 6.4‰) were distributed within the range of major anthropogenic sources (including NH3 and NO2 from coal combustion, vehicle exhausts and domestic wastes/sewage). At Menyuan site, δ15N values of PM2.5 (+8.0‰ to +27.9‰, +18.5 ± 5.8‰) were significantly higher than that of potential sources (including NH3 and NO2 from biomass burning, animal wastes, soil N cycle, fertilizer application and dust N). High molar ratios of to and/or in PM2.5 at the background site suggested that the equilibrium of NH3 ↔ caused apparent 15N enrichments in ammonium. Results of the SIAR model showed that 39 and 32% of bulk N in PM2.5 of Beijing site were contributed from N emissions of coal combustion and vehicle exhausts, respectively, whereas N in PM2.5 at Menyuan site was derived mainly from N emissions of biomass burning (46%) and NH3 volatilization (34%). These results revealed that the stoichiometry between NH3 and acidic gases plays an important role in controlling the bulk δ15N signatures of PM2.5 and emissions of reactive N from coal combustion and urban transportation should be strictly controlled to advert the risk of haze episodes in Beijing.","PeriodicalId":22320,"journal":{"name":"Tellus B: Chemical and Physical Meteorology","volume":"27 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2017-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"36","resultStr":"{\"title\":\"Source appointment of nitrogen in PM2.5 based on bulk δ15N signatures and a Bayesian isotope mixing model\",\"authors\":\"Yan-Li Wang, Xue‐Yan Liu, Wei Song, Wen Yang, B. Han, Xiaoyan Dou, Xu-Dong Zhao, Zhaoliang Song, Cong‐Qiang Liu, Z. 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At Menyuan site, δ15N values of PM2.5 (+8.0‰ to +27.9‰, +18.5 ± 5.8‰) were significantly higher than that of potential sources (including NH3 and NO2 from biomass burning, animal wastes, soil N cycle, fertilizer application and dust N). High molar ratios of to and/or in PM2.5 at the background site suggested that the equilibrium of NH3 ↔ caused apparent 15N enrichments in ammonium. Results of the SIAR model showed that 39 and 32% of bulk N in PM2.5 of Beijing site were contributed from N emissions of coal combustion and vehicle exhausts, respectively, whereas N in PM2.5 at Menyuan site was derived mainly from N emissions of biomass burning (46%) and NH3 volatilization (34%). 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引用次数: 36
摘要
氮同位素(δ15N)已被用于区分大气氮的主要来源,然而,基于大气样品中氮混合物的δ15N值来量化多种来源的贡献仍然是一个挑战。本研究测量了2013年1月22日至30日北京城市站点和2013年9月6日至10月15日中国西北青海省背景站点PM2.5中体氮的δ15N,然后应用贝叶斯同位素混合模型(SIAR, Stable isotope Analysis in R)分析了N源。北京站点PM2.5的δ15N值(−4.1‰~ +13.5‰,+2.8±6.4‰)分布在主要人为源(燃煤NH3和NO2、机动车尾气和生活垃圾/污水)范围内。在门源站点,PM2.5的δ15N值(+8.0‰~ +27.9‰,+18.5±5.8‰)显著高于潜在源(包括生物质燃烧产生的NH3和NO2、动物粪便、土壤N循环、施肥和粉尘N)。背景站点PM2.5中to和/或的高摩尔比表明NH3的平衡导致铵态氮明显富集。SIAR模型结果显示,北京站点PM2.5中散氮的39%和32%分别来自燃煤和机动车尾气的N排放,而门源站点PM2.5中的N主要来自生物质燃烧的N排放(46%)和NH3挥发(34%)。结果表明,NH3与酸性气体之间的化学计量在控制PM2.5的体δ15N特征中起重要作用,应严格控制燃煤和城市交通中活性N的排放,以降低北京雾霾的发生风险。
Source appointment of nitrogen in PM2.5 based on bulk δ15N signatures and a Bayesian isotope mixing model
Abstract Nitrogen isotope (δ15N) has been employed to differentiate major sources of atmospheric N. However, it remains a challenge to quantify contributions of multiple sources based on δ15N values of the N mixture in atmospheric samples. This study measured δ15N of bulk N in PM2.5 at an urban site of Beijing during a severe haze episode of 22–30 January 2013 and a background site of Qinghai, north-western China from 6 September to 15 October 2013, then applied a Bayesian isotope mixing model (SIAR, Stable Isotope Analysis in R) to analyse the N sources. At Beijing site, δ15N values of PM2.5 (−4.1‰ to +13.5‰, +2.8 ± 6.4‰) were distributed within the range of major anthropogenic sources (including NH3 and NO2 from coal combustion, vehicle exhausts and domestic wastes/sewage). At Menyuan site, δ15N values of PM2.5 (+8.0‰ to +27.9‰, +18.5 ± 5.8‰) were significantly higher than that of potential sources (including NH3 and NO2 from biomass burning, animal wastes, soil N cycle, fertilizer application and dust N). High molar ratios of to and/or in PM2.5 at the background site suggested that the equilibrium of NH3 ↔ caused apparent 15N enrichments in ammonium. Results of the SIAR model showed that 39 and 32% of bulk N in PM2.5 of Beijing site were contributed from N emissions of coal combustion and vehicle exhausts, respectively, whereas N in PM2.5 at Menyuan site was derived mainly from N emissions of biomass burning (46%) and NH3 volatilization (34%). These results revealed that the stoichiometry between NH3 and acidic gases plays an important role in controlling the bulk δ15N signatures of PM2.5 and emissions of reactive N from coal combustion and urban transportation should be strictly controlled to advert the risk of haze episodes in Beijing.