ISSN 1006-3021 CN11-3474/P
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含水层结构变异对区域地下水循环影响数值模拟
  
关键词:aquifer structural variation  group mining  groundwater  numerical simulation  Changzhi Basin
基金项目:国家自然科学基金重点项目(编号: 41130637);河北省高等学校科学技术研究项目(编号: ZD2014023; QN2015061);河北省科技计划项目(编号: 15273630);中国地质科学院水文地质环境地质研究所重点实验室开放基金(编号: KF201605)
作者单位E-mail
代锋刚 中国地质科学院岩溶地质研究所
河北地质大学, 河北省水资源可持续利用与开发重点实验室 
daifenggang@126.com 
张发旺 中国地质科学院岩溶地质研究所
中国地质科学院水文地质环境地质研究所 
zhangfawang@karst.ac.cn 
王滨 河北地质大学, 河北省水资源可持续利用与开发重点实验室  
么红超 中国地质科学院水文地质环境地质研究所  
陈立 中国地质科学院水文地质环境地质研究所  
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摘要:
Numerical Simulation of Structural Variation of Aquifer Effect on Regional Groundwater Circulation
      The destruction of groundwater resources caused by coal mining is the main bottleneck restricting the sustainable development of economy and environment in coal mining area. The contradiction between min-ing of coal resources and protection of water re-sources will become more serious. China's coal-rich regions are mainly distributed in north and northwest China. Only coal reserves in Shanxi, Inner Mongolia, Shaanxi and Xinjiang provinces account for 73.1% of the total coal reserves. Groundwater resources in these coal-rich areas are relatively poor. Severe water shortage accounted for 71% of key mining areas and 40% of serious water shortages. The serious damage to underground water resources exacerbated the shortage of water resources in the mining areas, which is particularly prominent in the energy province of Shanxi. The fundamental reason is that the mining caused structural changes in aquifers, resulting in damage to groundwater resources, so that the groundwater resources from the original quality of water available for exploitation into the pit of mine water and drain away, undermine the groundwater fill row, and destroyed the hydrological surface condi-tions, undermined the surface water cycle, thus af-fecting the regional groundwater cycle situation.
DAI Feng-gang,ZHANG Fa-wang,WANG Bin,YAO Hong-chao,CHEN Li.2017.Numerical Simulation of Structural Variation of Aquifer Effect on Regional Groundwater Circulation[J].Acta Geoscientica Sinica,38(s1):64-68.
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