Arsenic pollution in groundwater from Hetao Area, China

被引:47
作者
Zhang, H [1 ]
Ma, DS
Hu, XX
机构
[1] Najing Univ, State Key Lab Mineral Deposit Res, Nanjing 210093, Peoples R China
[2] Shanghai Jiao Tong Univ, Fac Environm Sci & Technol, Shanghai 200240, Peoples R China
来源
ENVIRONMENTAL GEOLOGY | 2002年 / 41卷 / 06期
关键词
arsenic pollution; China; groundwater; Hetao Area;
D O I
10.1007/s002540100442
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Hetao Area, China is a district where arsenic concentrations in drinking water are elevated. The 180,000 people that inhabit the 6,100 km(2) of the seven counties in the area show symptoms of arsenic poisoning. In this paper, the distribution and origin of arsenic in groundwater were studied. The results demonstrate that the affected district boundaries encompass an area with high contents of As in well water, which the local inhabitants drink and use in daily life. This district is labeled as a population pathological change area. The isotope ratios of Sr-87/Sr-86 (0.7100-0.7164), Pb-206/Pb-214 (18.3817-19.1871), and Pb-207/Pb-204 (15.7581-15.9578) in groundwater of the population pathological change area are close to the ratios measured in water from mine areas (Sr-87/Sr-86=0.7196, Pb-206/Pb-204=19.1940, Pb-217/Pb-214=15.9574), and are somewhat close to ratios in Yellow River, water which is used to irrigating in Hetao Area (Sr-117/Sr-86=0.7168, Pb-211/Pb-204=18.3495, Pb-207/Pb-204=15.5969). The average content of As in the drinking water is as high as four times more than the environmental standard of As in drinking water. The study suggests that the origin of the As in groundwater of the population pathological change area in Hetao Area is transported from higher elevations where mineral deposits exist. Mining of some of the deposits has occurred for a long time. Mining practices can result in release of toxic elements, which can then be transported from the mining district down gradient.
引用
收藏
页码:638 / 643
页数:6
相关论文
共 18 条
[1]  
[Anonymous], 1996, HYDROGEOLOGY ENG GEO
[2]  
*EPA INN MONG AUT, 1995, ENV QUAL REP 1995
[3]  
FARAGO ME, 1996, 39 INT GEOL C BEIJ, V3, P50
[4]   EFFECT OF PH ON ADSORPTION OF ARSENIC AND SELENIUM FROM LANDFILL LEACHATE BY CLAY-MINERALS [J].
FROST, RR ;
GRIFFIN, RA .
SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1977, 41 (01) :53-57
[5]  
KIM KW, 1996, 30 INT GEOL C BEIJ, V3, P45
[6]  
LINDA CD, 1991, ENVIRON SCI TECHNOL, V25, P420
[7]  
MOL WW, 1986, ANAL CHEM, V58, P113
[8]   Arsenic poisoning of Bangladesh groundwater [J].
Nickson, R ;
McArthur, J ;
Burgess, W ;
Ahmed, KM ;
Ravenscroft, P ;
Rahman, M .
NATURE, 1998, 395 (6700) :338-338
[9]   Mechanism of arsenic release to groundwater, Bangladesh and West Bengal [J].
Nickson, RT ;
McArthur, JM ;
Ravenscroft, P ;
Burgess, WG ;
Ahmed, KM .
APPLIED GEOCHEMISTRY, 2000, 15 (04) :403-413
[10]  
PARTRICK JP, 1994, WATER RESOUR RES, V30, P421