Study on hydrochemical characteristics and formation mechanism of shallow groundwater in eastern Songnen Plain
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  • 英文篇名:Study on hydrochemical characteristics and formation mechanism of shallow groundwater in eastern Songnen Plain
  • 作者:LI ; Xiao-han ; WANG ; Rui ; LI ; Jian-feng
  • 英文作者:LI Xiao-han;WANG Rui;LI Jian-feng;Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences;Team of Groundwater Resource Evaluation and Protection;School of Water Resources and Environment, Hebei GEO University;Hebei Province Key Laboratory of Sustained Utilization and Development of Water Resources;
  • 英文关键词:The Songnen Plain;;Groundwater;;Hydrochemical characteristics;;Hydrogeochemical modeling;;Formation
  • 中文刊名:DXSG
  • 英文刊名:地下水科学与工程(英文版)
  • 机构:Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences;Team of Groundwater Resource Evaluation and Protection;School of Water Resources and Environment, Hebei GEO University;Hebei Province Key Laboratory of Sustained Utilization and Development of Water Resources;
  • 出版日期:2018-09-15
  • 出版单位:Journal of Groundwater Science and Engineering
  • 年:2018
  • 期:v.6;No.22
  • 基金:supported by the fund from China Geological Survey Project (DD20160238);; Scientific Research Starting Foundation of Hebei GEO University (BQ201610);; Water Conservancy Scientific Research and Promotion Plan Project of Hebei Province (2017-58)
  • 语种:英文;
  • 页:DXSG201803001
  • 页数:10
  • CN:03
  • 分类号:4-13
摘要
Under the influence of global climate changes and human activities, the Songnen Plain's groundwater environment is deteriorating, which becomes an important factor restricting the social economic development and ecological balance. As a relatively independent water system in the Songnen Plain, the groundwater system of the Songhua River provides the main water sources for industry, agriculture, life and other aspects. According to the hydrogeological investigation, groundwater sample collection and testing in the eastern Songnen Plain, descriptive statistics analysis, piper diagram, Gibbs diagram and reverse hydrogeochemical simulation were used to analyze the hydrochemical characteristics and evolution laws of regional groundwater. The results of this study show that HCO_3~- and Ca~(2+) are the main anion and cation in the groundwater; the formation of groundwater chemical components are controlled by topographic and geomorphic factors and groundwater occurrence conditions; groundwater subarea of the Lalin-Ashi River is mainly controlled by weathering-dissolution process, and evaporation and ion-exchange reactions are more obvious in groundwater subarea of the Hulan-Tongken River, whose chemical composition also affects the valley plain groundwater subarea in the discharge area; in addition, local high intensity withdrawal causes abnormal hydrochemical evolution processes. The research results can offer scientific basis for rational utilization and protection of groundwater.
        Under the influence of global climate changes and human activities, the Songnen Plain's groundwater environment is deteriorating, which becomes an important factor restricting the social economic development and ecological balance. As a relatively independent water system in the Songnen Plain, the groundwater system of the Songhua River provides the main water sources for industry, agriculture, life and other aspects. According to the hydrogeological investigation, groundwater sample collection and testing in the eastern Songnen Plain, descriptive statistics analysis, piper diagram, Gibbs diagram and reverse hydrogeochemical simulation were used to analyze the hydrochemical characteristics and evolution laws of regional groundwater. The results of this study show that HCO_3~- and Ca~(2+) are the main anion and cation in the groundwater; the formation of groundwater chemical components are controlled by topographic and geomorphic factors and groundwater occurrence conditions; groundwater subarea of the Lalin-Ashi River is mainly controlled by weathering-dissolution process, and evaporation and ion-exchange reactions are more obvious in groundwater subarea of the Hulan-Tongken River, whose chemical composition also affects the valley plain groundwater subarea in the discharge area; in addition, local high intensity withdrawal causes abnormal hydrochemical evolution processes. The research results can offer scientific basis for rational utilization and protection of groundwater.
引文
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