摘要
针对渭北黄土原灌区地下水位上升问题，提出了地下水新含水层的概念。并以宝鸡峡、羊毛湾灌区为例，介绍了新含水层的分布及厚度，分析了新含水层的形式条件在此基础上，进行了地下水资源评价，进一步证明新含水层已构成渭北黄土原灌区巨大的地下水库。
With the problem of the underground water table rising in the irrigatedarea on the weibei Loess Highland,this paper suggests a concept of the underground wa-ter new aquifer.Taking Baoji Gorge and Yangmao Wuan irrigation systems for example,this paper analyses the distribution,thickness and forming conditions of this new aguiferon the basis of which an evaluation of the underground water resources in made,thus,confirming that this new aquifer has formed a huge underground reservoir in the irriga-tion system on he Weibei Loess Highland.
出处
《西北农业大学学报》
CSCD
1994年第1期1-6,共6页
Journal of Northwest Sci-Tech University of Agriculture and Forestry（Natural Science Edition)
关键词
灌区
地下水
含水层
渭北黄土原
new aquifer,underground water reservolr,storage water structure
