摘要
粘性土层在相邻含水层水文地质条件变化时,会引起其自身水文地质特性的变化而导致透水及释水。
Permeability may be induced to clayey soil as well as changes of hydrogeological properties may be incurred when the hydrogeological of condition the adjoining aquifer changes.
出处
《工程勘察》
CSCD
北大核心
1989年第1期30-32,共3页
Geotechnical Investigation & Surveying
