ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
华北平原地下水演变机制与调控
  
关键词:North China Plain  groundwater depression funnel  groundwater resources management
基金项目:国家重点基础研究计划(“973”)项目“华北平原地下水演变机制与调控”(编号: 2010CB428800)
作者单位E-mail
石建省 中国地质科学院水文地质环境地质研究所 tiger7886@263.net 
李国敏 中国科学院地质与地球物理研究所  
梁杏 中国地质大学(武汉)  
陈宗宇 中国地质科学院水文地质环境地质研究所  
邵景力 中国地质大学(北京)  
宋献方 中国科学院地理科学与资源研究所  
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摘要:
Evolution Mechanism and Control of Groundwater in the North China Plain
      The long-term overexploitation of groundwater in the North China Plain has produced complicated groundwater depression funnels and caused a series of environmental problems. To realize the harmonization between the regional economic development and the groundwater resources and environment, researchers have implemented since 2010 the project “Evolution Mechanism and Management of the Groundwater in North China”, which is a National Basic Research Program (973) of China. On the basis of numerous previous studies, the evolution of groundwater flowing field and its response to human activities in the past 50 years were analyzed, and the change of water flowing parameters and the structure of vadose zone were investigated. The evolution of ground depression, the movement of saline water bodies, and the composition of deep groundwater were studied. A high resolution numerical groundwater flow model was built up based on renewed data between 2001 and 2010 and improved groundwater modeling technologies. Based on this model, the authors calculated the up-to-date amount of groundwater resources. The groundwater resources carrying capacities (GRCC) were assessed and the main factors affecting the GRCC were analyzed. The optimizing solutions for the management of the groundwater resources in the North China Plain were put forward and were modeling by the newly-built high resolution groundwater flow model.
SHI Jian-sheng,LI Guo-min,LIANG Xing,CHEN Zong-yu,SHAO Jing-li,SONG Xian-fang.2014.Evolution Mechanism and Control of Groundwater in the North China Plain[J].Acta Geoscientica Sinica,35(5):527-534.
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