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.
引用
收藏
页数:17
相关论文
共 50 条
  • [41] Tectonic evolution and controls on natural gas generation and accumulation in the Ordovician system of the Ordos Basin, North China
    Yang, Peng
    Ren, Zhanli
    Zhou, Renjie
    Cui, Junping
    Qi, Kai
    Fu, Jinhua
    Li, Jinbu
    Liu, Xinshe
    Li, Wenhou
    Wang, Kun
    [J]. ENERGY REPORTS, 2021, 7 : 6887 - 6898
  • [42] Evolution of coal structures: FTIR analyses of experimental simulations and naturally matured coals in the Ordos Basin, China
    Yao, Suping
    Zhang, Ke
    Jiao, Kun
    Hu, Wenxuan
    [J]. ENERGY EXPLORATION & EXPLOITATION, 2011, 29 (01) : 1 - 19
  • [43] Pressure compartment and evolution of reservoir porosity in the Upper Paleozoic of Daniudi Gas Field, Ordos Basin, China
    Li, Zhong-Dong
    Zhang, Shao-Nan
    Zhou, Wen
    Hui, Kuan-Yang
    Li, Liang
    Guo, Min
    Fan, Shi-Long
    Yuan, Jing-Su
    [J]. Kuangwu Yanshi, 2007, 27 (03): : 73 - 80
  • [44] Geochemical characteristics, generation, and evolution mechanism of coalbed methane in the south-western Ordos Basin, China
    Lin, Yabing
    Qin, Yong
    Ma, Dongmin
    Wang, Shengquan
    [J]. FRONTIERS OF EARTH SCIENCE, 2024, 18 (02) : 296 - 311
  • [45] Dolomitization of the Ordovician subsalt Majiagou Formation in the central Ordos Basin, China: fluid origins and dolomites evolution
    Xiong, Ying
    Wang, Li-Chao
    Tan, Xiu-Cheng
    Liu, Yun
    Liu, Ming-Jie
    Qiao, Zhan-Feng
    [J]. PETROLEUM SCIENCE, 2021, 18 (02) : 362 - 379
  • [46] Paleogeographic and sedimentary evolution of Meso-Neoproterozoic strata in the Ordos Basin, western North China Craton
    Bai, Jinli
    Zhao, Junfeng
    Ren, Zhanli
    Li, Wenhou
    Wang, Ke
    Li, Xuan
    [J]. JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING, 2022, 215
  • [47] The coupling mechanism of basin and orogen in the western Ordos Basin and adjacent regions of China
    Liu, SF
    [J]. JOURNAL OF ASIAN EARTH SCIENCES, 1998, 16 (04) : 369 - 383
  • [48] Hydrogeochemistry evidence of groundwater circulation features in Ordos Cretaceous basin-A Case Study in Chabu well field
    Sun, Fang-Qiang
    Hou, Guang-Cai
    Dou, Yan
    Fang, Chang-Sheng
    Jiang, Jun
    Zhang, Le-Zhong
    [J]. Jilin Daxue Xuebao (Diqiu Kexue Ban)/Journal of Jilin University (Earth Science Edition), 2009, 39 (02): : 269 - 275
  • [49] Hydrogeochemistry, Geothermometry, and Genesis of the Hot Springs in the Simao Basin in Southwestern China
    Zhang, Yuqi
    Zhou, Xun
    Liu, Haisheng
    Yu, Mingxiao
    Hai, Kuo
    Tan, Mengru
    Huo, Dongxue
    [J]. GEOFLUIDS, 2019, 2019
  • [50] Hydrogeochemistry of high-fluoride groundwater at Yuncheng Basin, northern China
    Li, Chengcheng
    Gao, Xubo
    Wang, Yanxin
    [J]. SCIENCE OF THE TOTAL ENVIRONMENT, 2015, 508 : 155 - 165