摘要
本文从地下水与河水的水流形态和水位动态变化 ,分析了二者的补排关系 ;详细介绍了地形地貌、水文地质、气候和人为因素等对地下水与河水相互作用的影响 ;综述了研究地下水与河水相互作用的研究方法 ,如野外实验和室内实验方法、动态资料分析方法、基流切割方法、水化学方法、地下水动力学方法等 ;评述了研究河流与含水层相互作用的解析模型和数值模型的发展状况。最后 ,指出多种方法的相互验证、数学模型中补排量和边界的处理、地下水与河水交错带的研究、河流与含水层相互作用的生态意义、加强相关学科的交流与合作将是未来的发展方向。
The interaction between groundwater and streams is very important in water science. In this paper, the authors reviewed the development of the interaction of streams and groundwater in the following aspects. a. The principle of recharge and discharge between groundwater and streams was analyzed by investigating the changes in water flow and water table. b. Some factors that effect the interaction of groundwater and streams were illustrated, such as topography, hydrogeology, climate and other anthropogenic influence. c. Some study methods were assessed, such as field and laboratory experiment, dynamic data analysis, water chemistry. d. The development of modeling the interaction of aquifer and streams was discussed. The authors pointed out that some research fields will become frontiers and of concern, such as ecological significance of interaction of groundwater and stream, anthropogenic influence and hydrogeology of hyprotheic zone, multi-disciplinary communication and cooperation.
出处
《水文地质工程地质》
CAS
CSCD
2004年第1期108-113,共6页
Hydrogeology & Engineering Geology
基金
国家重点基础研究发展规划项目 (G19990 43 60 6)
国家自然科学基金委员会
水利部黄河水利委员会黄河联合资助项目 (5 0 2 3 90 10 )
关键词
地下水
河水
水流形态
水位动态变化
groundwater
stream
interaction of groundwater and stream
research development