Evolution of Hydrogeochemistry in the Haolebaojinao Watershed of the Ordos Basin, China

被引:3
|
作者
Zhang, Baoyun [1 ]
Zhang, Ruolin [2 ]
Han, Peng-Fei [3 ,4 ,5 ]
Wang, Junzhi [6 ,7 ]
Wan, Li [3 ,4 ,5 ]
机构
[1] Chinese Acad Geol Sci, Inst Geophys & Geochem Explorat, Langfang 065000, Peoples R China
[2] China Inst Geoenvironm Monitoring, Beijing 100081, Peoples R China
[3] China Univ Geosci, Key Lab Groundwater Conservat, Minist Water Resources, Beijing 100083, Peoples R China
[4] China Univ Geosci, Key Lab Groundwater Circulat & Environm Evolut, Minist Educ, Beijing 100083, Peoples R China
[5] China Univ Geosci, Sch Water Resources & Environm, Beijing 100083, Peoples R China
[6] Yellow River Engn Consulting Co Ltd YREC, Zhengzhou 450003, Peoples R China
[7] Minist Water Resources Construct, Key Lab Water Management & Water Secur Yellow Rive, Zhengzhou 450003, Peoples R China
关键词
water chemistry process; water-rock interaction; Ordos Basin; basin water cycle; isotope; GROUNDWATER-FLOW SYSTEMS; LAKE BASIN; RECHARGE; AREA; AQUIFERS; QUALITY; IDENTIFICATION; INTRUSIONS; ISOTOPES; PART;
D O I
10.3390/su15065091
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The exploitation of groundwater in arid and semi-arid areas, especially in basins where groundwater is intensively exploited, is likely to have adverse effects on the originally fragile ecological environment, which also greatly alter the hydrogeochemical evolution process. Over-abstraction of groundwater in the Haolebaoji watershed of the Ordos Basin located in the semi-arid regions has led to a series of changes in the groundwater system, which has attracted considerable attention from environmental protection organizations. However, the origin and geochemical evolution of groundwater in the Haolebaoji watershed have not been revealed. In this study, the Haolebaoji watershed is selected as the typical study area to investigate hydrogeochemical evolution under the intensive groundwater exploitation. Groundwater samples were collected and tested for major ions and stable isotopes (delta O-18, delta D). Various approaches including the ion proportional relationship diagram, chlor-alkali index, saturation index, Gibbs diagram, and principal factor analysis were used to reveal the hydrogeochemical processes regulating the groundwater geochemistry. The groundwater in the study area is divided into five hydrochemical types according to the Piper diagram. It was found that the chemical composition of groundwater in the study area is mainly controlled by the dissolution of calcite, dolomite, gypsum, and halite. The cation exchange intensity gradually increased with the flow of groundwater from the recharge to the discharge area. Rock weathering plays a controlling role in the formation of groundwater geochemistry, but it is also controlled by evaporative crystallization in some runoff and discharge areas. Groundwater is predominantly recharged by modern local atmospheric precipitation, and deep wells receive water supply during cold periods. The study findings provide important information for the development of sustainable groundwater management strategies for the Ordos Energy Base.
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页数:17
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