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Evolution of aerosol chemistry in Xi'an, inland China, during the dust storm period of 2013-Part 1: Sources, chemical forms and formation mechanisms of nitrate and sulfate
Wang, GH (Wang, G. H.)[ 1,2 ]; Cheng, CL (Cheng, C. L.)[ 1,3 ]; Huang, Y (Huang, Y.)[ 1,3 ]; Tao, J (Tao, J.)[ 4 ]; Ren, YQ (Ren, Y. Q.)[ 1,3 ]; Wu, F (Wu, F.)[ 1 ]; Meng, JJ (Meng, J. J.)[ 1,3 ]; Li, JJ (Li, J. J.)[ 1 ]; Cheng, YT (Cheng, Y. T.)[ 1,3 ]; Cao, JJ (Cao, J. J.)[ 1 ]; Liu, SX (Liu, S. X.)[ 1 ]; Zhang, T (Zhang, T.)[ 1 ]; Zhang, R (Zhang, R.)[ 1 ]; Chen, YB (Chen, Y. B.)[ 1 ]
2014
Source PublicationATMOSPHERIC CHEMISTRY AND PHYSICS
Volume14Issue:21Pages:11571-11585
Subtype期刊论文
Abstract

A total suspended particulate (TSP) sample was collected hourly in Xi'an, an inland megacity of China near the Loess Plateau, during a dust storm event of 2013 (9 March 18: 00-12 March 10: 00 LT), along with a size-resolved aerosol sampling and an online measurement of PM2.5. The TSP and size-resolved samples were determined for elemental carbon (EC), organic carbon (OC), water-soluble organic carbon (WSOC) and nitrogen (WSON), inorganic ions and elements to investigate chemistry evolution of dust particles. Hourly concentrations of Cl-, NO3-, SO42-, Na+ and Ca2+ in the TSP samples reached up to 34, 12, 180, 72 and 28 mu g m(-3), respectively, when dust peak arrived over Xi'an. Chemical compositions of the TSP samples showed that during the whole observation period NH4+ and NO3- were linearly correlated with each other (r(2) = 0.76) with a molar ratio of 1 : 1, while SO42- and Cl- were well correlated with Na+, Ca2+, Mg2+ and K+ (r(2) > 0.85). Size distributions of NH4+ and NO3- presented a same pattern, which dominated in the coarse mode (>2.1 mu m) during the event and predominated in the fine mode (<2.1 mu m) during the non-event. SO42- and Cl- also dominated in the coarse mode during the event hours, but both exhibited two equivalent peaks in both the fine and the coarse modes during the non-event, due to the fine-mode accumulations of secondarily produced SO42- and biomass-burning-emitted Cl- and the coarse-mode enrichments of urban soil-derived SO42- and Cl-. Linear fit regression analysis further indicated that SO42- and Cl- in the dust samples possibly exist as Na2SO4, CaSO4 and NaCl, which directly originated from Gobi desert surface soil, while NH4+ and NO3- in the dust samples exist as NH4NO3. We propose a mechanism to explain these observations in which aqueous phase of dust particle surface is formed via uptake of water vapor by hygroscopic salts such as Na2SO4 and NaCl, followed by heterogeneous formation of nitrate on the liquid phase and subsequent absorption of ammonia. Our data indicate that 54 +/- 20% and 60 +/- 23% of NH4+ and NO3- during the dust period were secondarily produced via this pathway, with the remaining derived from the Gobi desert and Loess Plateau, while SO42- in the event almost entirely originated from the desert regions. Such cases are different from those in the East Asian continental outflow region, where during Asia dust storm events SO42- is secondarily produced and concentrates in sub-micrometer particles as (NH4)(2)SO4 and/or NH4HSO4. To the best of our knowledge, the current work for the first time revealed an infant state of the East Asian dust ageing process in the regions near the source, which is helpful for researchers to understand the panorama of East Asian dust ageing process from the desert area to the downwind region.

DOI10.5194/acp-14-11571-2014
Indexed BySCI
Language英语
Citation statistics
Cited Times:13[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.ieecas.cn/handle/361006/9797
Collection粉尘与环境研究室
Corresponding AuthorWang, GH (Wang, G. H.)[ 1,2 ]
Affiliation1.State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences,Xi’an 710075, China;
2.School of Human Settlements and Civil Engineering, Xi’an Jiaotong University, Xi’an 710079, China;
3.University of Chinese Academy of Sciences, Beijing 100049, China;
4.South China Institute of Environmental Science, Guangzhou 510655, China
Recommended Citation
GB/T 7714
Wang, GH ,Cheng, CL ,Huang, Y ,et al. Evolution of aerosol chemistry in Xi'an, inland China, during the dust storm period of 2013-Part 1: Sources, chemical forms and formation mechanisms of nitrate and sulfate[J]. ATMOSPHERIC CHEMISTRY AND PHYSICS,2014,14(21):11571-11585.
APA Wang, GH .,Cheng, CL .,Huang, Y .,Tao, J .,Ren, YQ .,...&Chen, YB .(2014).Evolution of aerosol chemistry in Xi'an, inland China, during the dust storm period of 2013-Part 1: Sources, chemical forms and formation mechanisms of nitrate and sulfate.ATMOSPHERIC CHEMISTRY AND PHYSICS,14(21),11571-11585.
MLA Wang, GH ,et al."Evolution of aerosol chemistry in Xi'an, inland China, during the dust storm period of 2013-Part 1: Sources, chemical forms and formation mechanisms of nitrate and sulfate".ATMOSPHERIC CHEMISTRY AND PHYSICS 14.21(2014):11571-11585.
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