摘要
位于骊山的明圣宫滑坡是一个古滑坡 ,在现场调查的基础上 ,为进行稳定性评价 ,对滑坡的形成条件进行了详细的研究 ,明圣宫滑坡活动的原因是地层、大气降水、地下水、地貌条件、滑动带贯通、拉张裂隙形成等综合因素作用的结果。应用极限平衡法进行分析得知 ,明圣宫滑坡已处于不稳定状态而必须及时整治 。
the Mingshenggong landslide, which lies in Lishan mountain, is an old landslide. In order to study the stability of the Mingshenggong landslide, the authors study in details the formation condition based on the plot investigation. The Mingshenggong landslide is caused by synthetic factors, such as layers, precipitation, ground water, physiognomy, slipping belt and crannies. According to the limit balance method, the Mingshenggong landslide is under an instability situation and has to be dealt with promptly.
出处
《水土保持通报》
CSCD
北大核心
2002年第3期25-27,共3页
Bulletin of Soil and Water Conservation
基金
中国科学院知识创新工程重大项目"西部生态环境演变规律与水土资源可持续利用研究"(KZCX1-10 -0 4)
陕西省自然科学基金项目"黄土高原植被重建过程中的水文效应研究"(2 0 0 0 D0 8)
