摘要
本文通过对基岩水与孔隙水的比较分析，介绍了基岩水的分布、水动力学和水化学特征，指出了基岩水运动具有均位趋势、选择流动及汇流特性，得出了渗流理论不宜用于基岩水的结论。
This paper,based on the comparison and analysis between bedrock water and pore water,puts forward the distribution, hydrodynamical and hydrochemical properties of bedrock water, points out that the movement of bedrock water is characterized by the tendency of uniforrn level,selective flow and confluence,and draws the conclusion that the seepage theory is not applicable to bedrock water.
出处
《水文地质工程地质》
CAS
CSCD
1997年第3期15-17,共3页
Hydrogeology & Engineering Geology
基金
煤炭部科研基金
关键词
基岩水
壁间运动
均位趋势
选择流动
孔隙水
bedrock water, interwall movement, tendency of uniform level, selective flow
