Stable hydrogen isotope composition of n-alkanes in urban atmospheric aerosols in Taiyuan, China
Stable hydrogen isotope composition of n-alkanes in urban atmospheric aerosols in Taiyuan, China
复制标题
太原城市大气气溶胶中正构烷烃的稳定氢同位素组成
DOI:
10.1016/j.atmosenv.2017.01.028
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发表时间:
2017-03
影响因子:
5
通讯作者:
Ling Mu
中科院分区:
文献类型:
--
作者:
Huiling Bai;Yinghui Li;Lin Peng;Xiangkai Liu;Xiaofeng Liu;Chongfang Song;Ling Mu
The hydrogen isotope compositions (δD) ofn-alkanes associated with particulate matter with a diameter of ≤10 μm from Taiyuan, China, during heating and non-heating periods were measured via gas chromatography–isotope ratio mass spectrometry to reveal the spatial and temporal characteristics of five functional zones and to provide another constraint on atmospheric pollutants. TheδD values ofn-C16ton-C31during the heating and non-heating periods ranged from −235.9‰ to −119.8‰ and from −231.3‰ to −129.2‰, respectively, but these similar spans had different distribution features. During the heating period, theδD distributions between non–central heating and commercial districts were consistent, as were those between residential and industrial districts; then-alkanes came from two or more types of emission sources. Coal soot might be the primary local emission source, but not the only source. During the non-heating period, then-alkanes ofn-C16ton-C20were more depleted in D with the increasing carbon number in all functional zones, but there was no rule forn-C21ton-C31. Specifically, coal soot and vehicle exhaust might be the primary sources ofn-alkanes for non–central heating districts in the heating and non-heating periods, respectively, according to theδD distribution ofn-C18ton-C22; gasoline vehicle exhaust might be ann-alkane source, and the hydrogen isotope fractionation effect during the condensation process should be a pollution mechanism for the commercial district during the heating period; theδD distribution difference ofn-C16ton-C18between the two periods in the residential and industrial districts was consistent, which indicates a similar source of fossil fuel combustion and a similar isotope fractionation effect during the non-heating period.
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影响因子:
5.5
作者:
Junji Cao;Xiaofeng Liu;Jianqiang Zhang;Ling Mu
通讯作者:
Ling Mu
影响因子:
5.2
作者:
T. Umezawa;T. Machida;S. Aoki;T. Nakazawa
通讯作者:
T. Umezawa;T. Machida;S. Aoki;T. Nakazawa
影响因子:
5
作者:
D. Widory;Stéphane Roy;Y. Moullec;G. Goupil;A. Cocherie;C. Guerrot
通讯作者:
D. Widory;Stéphane Roy;Y. Moullec;G. Goupil;A. Cocherie;C. Guerrot
影响因子:
5
作者:
E. Schefuß;V. Ratmeyer;J. Stuut;J. Jansen;Jaap S. Sinninghe Damsté
通讯作者:
E. Schefuß;V. Ratmeyer;J. Stuut;J. Jansen;Jaap S. Sinninghe Damsté
影响因子:
3.4
作者:
Yi Wang;Y. Huang
通讯作者:
Yi Wang;Y. Huang