Geothermal spring causes arsenic contamination in river waters of the southern Tibetan Plateau, China

被引:0
作者
Chaoliu Li
Shichang Kang
Pengfei Chen
Qianggong Zhang
Jue Mi
Shaopeng Gao
Mika Sillanpää
机构
[1] Chinese Academy of Sciences,State Key Laboratory of Cryospheric Sciences
[2] Institute of Tibetan Plateau Research,Key Laboratory of Tibetan Environment Changes and Land Surface Processes
[3] Chinese Academy of Sciences,Laboratory of Green Chemistry
[4] Graduate University of Chinese Academy of Sciences,Key Laboratory of Tibetan Environment Changes and Land Surface Processes
[5] People’s Government,undefined
[6] Lappeenranta University of Technology,undefined
[7] Institute of Tibetan Plateau Research,undefined
[8] Chinese Academy of Sciences,undefined
来源
Environmental Earth Sciences | 2014年 / 71卷
关键词
Tibetan Plateau; Lhasa River; Arsenic; Water quality; Geothermal spring;
D O I
暂无
中图分类号
学科分类号
摘要
Large numbers of As-enriched geothermal springs are distributed at the southern Tibetan Plateau, and their influence on river water is still not clear. Lhasa River and its tributary, Duilong Qu located at downstream of the largest geothermal spring of the Tibetan Plateau, were selected for sampling during monsoon and non-monsoon seasons. Dissolved trace elements (B, Cr, Ni, Cu, Zn, As, Cs, Ba and U) were measured in river water samples by ICP-MS. The results show that due to contribution of geothermal spring, As levels of Duilong Qu (205.6 μg/L) and Lhasa River (12.7 μg/L) were higher during non-monsoon season than that of WHO guideline for drinking water (10 μg/L). Accordingly, As level of river water was lower during the monsoon season than that of the non-monsoon season due mainly to dilution process. Therefore, although Tibetan rivers are generally considered as free of contamination, geothermal springs cause As contamination of river water at some local regions and may harm the local residents. Further research is needed in other parts of the plateau to determine whether As level of groundwater of the related region is high.
引用
收藏
页码:4143 / 4148
页数:5
相关论文
共 107 条
[1]  
Ahmed F(2010)Geochemical study of arsenic and other trace elements in groundwater and sediments of the Old Brahmaputra River Plain, Bangladesh Environ Earth Sci 60 1303-1316
[2]  
Bibi MH(2011)Diagnosis of stream sediment quality and assessment of toxic element contamination sources in East Attica, Greece Environ Earth Sci 63 1369-1383
[3]  
Ishiga H(2009)Heavy metals and polychlorinated biphenyls in sediments of the Yangtze river estuary, China Environ Earth Sci 59 363-370
[4]  
Fukushima T(2009)Arsenic fractionation in sediments of different origins using BCR sequential and single extraction methods J Hazard Mater 167 745-751
[5]  
Maruoka T(2002)Drinking water, and health: a position paper of the American Council on Science and Health Regul Toxicol Pharm 36 162-174
[6]  
Alexakis D(2006)Metal speciation in coastal marine sediments from Singapore using a modified BCR-sequential extraction procedure Appl Geochem 21 1335-1346
[7]  
An Q(2011)Seasonal variations of Zn, Cu, As and Mo in arsenic-rich stream at the Mokrsko gold deposit, Czech Republic Environ Earth Sci 62 429-441
[8]  
Wu Y(2012)Anthropogenic arsenic menace in Delhi Yamuna Flood Plains Environ Earth Sci 65 131-139
[9]  
Wang J(2012)Geochemistry and mineralogy of surface pyritic tailings impoundments at two mining sites of the Iberian Pyrite Belt (SW Spain) Environ Earth Sci 65 669-680
[10]  
Li Z(2008)B, As, and F Contamination of river water due to wastewater discharge of the Yangbajing geothermal power plant, Tibet, China Environ Geol 56 197-205