Hydrogeochemical characteristics and evolution of the aquifer systems of Gonghe Basin, Northern China

被引：27

作者：

Cao, Wen-Geng ^{[1
,2
]}

Yang, Hui-Feng ^{[2
]}

Liu, Chun-Lei ^{[2
]}

Li, Yuan-Jie ^{[3
]}

Bai, Hua ^{[2
]}

机构：

[1] North China Univ Water Resources & Elect Power, Zhengzhou 45001L, Henan, Peoples R China

[2] Chinese Acad Geol Sci, Inst Hydrogeol & Environm Geol, Shijiazhuang 050061, Hebei, Peoples R China

[3] Inner Mongolia Geol Environm Monitoring, Hohot 010020, Peoples R China

来源：

GEOSCIENCE FRONTIERS | 2018年 / 9卷 / 03期

基金：

中国国家自然科学基金;

关键词：

Hydrogeochemical characteristics; Gonghe Basin; Ionic ratio; Ion-exchange; Groundwater quality; GROUNDWATER; AREA; SPRINGS; TUSCANY;

D O I：

10.1016/j.gsf.2017.06.003

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

We present the first systematic hydrogeological analysis to grain insights on the evolution of the Gonghe Basin in North China. Two hundred and forty seven water samples were collected from the Gonghe East Basin, Gonghe West Basin and Chaka Basin. The three groundwater systems of Gonghe Basin from west to east display different geochemical signatures. Based on Na/Cl ratios and Langelier-Ludwig diagram, it is inferred that the groundwater recharge potential of the Gonghe East Basin is much prosperous than the other areas. The renewability of the aquifers in alluvial-proluvial fan of Wahonghe and Gonghe East Basin margin is much faster than in the other basins. The groundwater quality in Chaka Salt Lake, Shazhuyu and Qiabuqia River Valley plains is low due to strong evaporation and cation exchange. The groundwater quality of the phreatic aquifers in the Qiabuqia River Valley plain is further deteriorated by mixing of high-arsenic and high-mineralization water from the deep fault structures. (C) 2018, China University of Geosciences (Beijing) and Peking University. Production and hosting by Elsevier B.V. This is an open access article under the CC BY-NC-ND license.

引用

页码：907 / 916

页数：10

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