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层状岩质边坡地下水分布特征及其控稳作
引用本文:陈志坚,吉林.层状岩质边坡地下水分布特征及其控稳作[J].河海大学学报(自然科学版),2001,29(1):107-110.
作者姓名:陈志坚  吉林
作者单位:河海大学土木工程学院,
基金项目:国家“八五”科技攻关项目(208-03-02(3-2-5))
摘    要:在阐述层状岩质边坡岩性组合分类和地下水分布特征的基础上,介绍了考虑残坡积层孔隙水和裂隙潜水控稳作用的边坡稳定性计算方法,根据小浪底水利枢纽工程若干边坡有的有限元计算,结果表明:考虑包气带裂隙水作用时,边坡安全系数可降低5%-15%;当库水位聚降时,裂隙潜水对边坡稳定性也有重要影响。

关 键 词:层状岩体  边坡  稳定性  有限元  地下水
文章编号:1000-1980(2001)01-0107-04
修稿时间:1999年11月2日

Distribution Character and Stability Controlling Effect of Underground Water in Layered Rock Slope
CHEN Zhi-jian,Ji Lin.Distribution Character and Stability Controlling Effect of Underground Water in Layered Rock Slope[J].Journal of Hohai University (Natural Sciences ),2001,29(1):107-110.
Authors:CHEN Zhi-jian  Ji Lin
Abstract:On the basis of the combination and classification of the lithological character and the feature of underground water distribution, a slope stability calculation method is introduced, which includes the effect of pore water in the eluvial slope, fissure water in the aerated zone and fissure phreatic water. The finite element calculation for many slopes of Xiaolangdi Multipurpose Dam Project proves that the safety factor will reduce by 5%~15% when fissure water in the aerated zone is considered and that fissure phreatic water has a large effect on the slope stability when the reservoir water level falls suddenly.
Keywords:
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