Hydrogeochemistry of high arsenic groundwater from Hangjinhouqi of Hetao Plain, Inner Mongolia
High arsenic groundwaters at Hangjinhouqi of Hetao plain were investigated. The major hydrochemical types of most saline groundwaters are Cl-HCO3-Na-Mg and Cl-Na-Mg. By contrast, fresh groundwaters generally belong to HCO3-Na-Mg type. High concentrations of As in shallow aquifers are associated with strongly reducing conditions, evidenced by high concentrations of DOC, dissolved Fe, dominance of As (Ⅲ), relatively low concentrations of NO3 and SO4, and occasionally high content of dissolved CH4.
Y.Deng Y.Wang T.Ma
School of Environmental Studies and MOE Key Laboratory of Biogeology and Environmental Geology, China;University of Geosciences, Wuhan, China
国际会议
第十二届水-岩相互作用国际研讨会(P0roceedings of the 12th International Symposium on Water-Rock Interaction)
昆明
英文
1037-1041
2007-07-31(万方平台首次上网日期,不代表论文的发表时间)