摘要
河西走廊自南部山区至北部平原,地下水与河水之间形成有规律的、大量的重复转化过程。本文对河西走廊的水资源从祁连山中高山形成区到下游盆地湖积平原的消失区,地下水与河水之间经过几个不同地带的转化进行了论述,阐述了相互转化的关系及规律。
From south mountainous area to north dant transformation process has been formed between plain of Hexi Corridor, a repeated, regular and abungroundwater and river water. This paper discusses the transformation of groundwater and river water through several different belts of Hexi Corridor, which are from forming area of Qilian Mountain to disappearing area of lacustrine deposit plain in lower reaches basin, and expatiates on the relationship and rule of mutual transformation.
出处
《地下水》
2005年第4期256-259,共4页
Ground water
关键词
地表水
地下水
Surface Water, Groundwater, Relationship of Transformation