黄土高原缺水的地质环境及找水环境

文章分析了黄土高原地下水形成的地质环境，认为降水量、地形地貌、岩性构造和地下水循环是造成黄土高原产重缺水的主要因素，地层岩性和新构造运动是影响地下水富集的决定性因素。指出黄土高原基岩风化带潜水的相对富水岩组和富水地段，提出研究含水层的岩性和构造，寻找基岩风化带潜水是解决黄土高原局部地段缺水的较好途径。

Geological environment deficient in water and way to seek water in the loess plateau

The geological environment for the formation of groundwater in the Loess plateau has been analyzed in the paper.The author holds that the main factors to cause the serious shortage of water in the Loess plateau are rainfall, landform, strata structure and groundwater circulation, and the strata lithology and neotectonic movement are the decisive factors affecting the groundwater environment. The relatively water-enriched formation and water-enriched area for phreatic water in the basement weathering zone of the Loess plateau has been determined. In conclusion the author has put forward that the better way for solving the local shortage of water in the Loess plateau is to study the lithology and structure of the aquifer and to seek phreatic water in the basement weathering Zone.