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Concentration, sources, and flux of dissolved organic carbon of precipitation at Lhasa city, the Tibetan Plateau
Li, CL (Li, Chaoliu)1,3; Yan, FP (Yan, Fangping)2,4; Kang, SC (Kang, Shichang)2,3; Chen, PF (Chen, Pengfei)1,4; Qu, B (Qu, Bin)5; Hu, ZF (Hu, Zhaofu)2,4; Sillanpaa, M (Sillanpaa, Mika)5; Li, CL
Source PublicationENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH
2016
Volume23Issue:13Pages:12915-12921
DOI10.1007/s11356-016-6455-1
AbstractDissolved organic carbon (DOC) plays an important role in the climate system, but few data are available on the Tibetan Plateau (TP). In this study, 89 precipitation samples were collected at Lhasa, the largest city of southern Tibet, from March to December 2013. The average concentration and wet deposition flux of DOC was 1.10 mg C L-1 and 0.63 g C m(-2) year(-1), respectively. Seasonally, low DOC concentration and high flux appeared during the monsoon period, which were in line with heavy precipitation amount, reflecting dilution effect of precipitation for the DOC. Compared to other regions, the values of Lhasa were lower than those of large cities (e.g., Beijing and Seoul) mainly because of less air pollution of Lhasa. The principal component analysis (PCA) of DOC and ions (Ca2+, Mg2+, Na+, K+, NH4+, Cl-, NO3-, and SO42-) showed that DOC of Lhasa was derived mainly from the natural sources, followed by anthropogenic burning activities. Furthermore, Delta C-14 value of DOC indicated that fossil fuel combustion contributed around 28 % of the rainwater DOC of Lhasa, indicating that the atmosphere of Lhasa has been influenced by emission from fossil fuel combustion or high-temperature industrial processes.
Subject Area自然地理学
WOS IDWOS:000378817300031
Language英语
Indexed BySCI
KeywordSeasonal-variations Atmospheric Circulation Elemental Composition Light-absorption Wet Deposition Trace-elements Black Carbon Ice Cores Aerosols China
Cooperation Status国际
Department环境
SubtypeArticle
Citation statistics
Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/7669
Collection图书馆
Corresponding AuthorLi, CL
Affiliation1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Tibetan Environm Changes & Land Surface P, Beijing 100101, Peoples R China
2.Cold & Arid Reg Environm & Engn Res Inst CAS, State Key Lab Cryospher Sci, Lanzhou 730000, Peoples R China
3.Chinese Acad Sci, CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
4.Grad Univ Chinese Acad Sci, Beijing 100039, Peoples R China
5.Lappeenranta Univ Technol, Lab Green Chem, Sammonkatu 12, FIN-50130 Mikkeli, Finland
Recommended Citation
GB/T 7714
Li, CL ,Yan, FP ,Kang, SC ,et al. Concentration, sources, and flux of dissolved organic carbon of precipitation at Lhasa city, the Tibetan Plateau[J]. ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH,2016,23(13):12915-12921.
APA Li, CL .,Yan, FP .,Kang, SC .,Chen, PF .,Qu, B .,...&Li, CL.(2016).Concentration, sources, and flux of dissolved organic carbon of precipitation at Lhasa city, the Tibetan Plateau.ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH,23(13),12915-12921.
MLA Li, CL ,et al."Concentration, sources, and flux of dissolved organic carbon of precipitation at Lhasa city, the Tibetan Plateau".ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH 23.13(2016):12915-12921.
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