凤滩库岸的稳定性研究  

Discussion on the Fengtan Bank Stability

作　　者：周中民[1] 左利芳[2] 

机构地区：[1]长沙电力学院环境工程及生物技术研究所,湖南长沙410077 [2]长沙电力学院现代教育技术中心,湖南长沙410077

出　　处：《长沙水电师院学报（自然科学版）》2001年第4期84-86,共3页

摘　　要：滑坡 ,是坡地后退过程中的一个明显标志 .属于坡地之一的凤滩水库库岸 ,也有一些不稳定现象 ,但并非都是滑坡 .有的是沿着节理发育的深切溪沟溯源侵蚀 ,其源头已经伸入到了河流阶地之中 ,使阶地面遭受切割 ;有的是阶地面被数条溪沟分割之后 ,胜似滑坡而非滑坡 ;有的是残积坡积层沿着阶地前缘斜坡的部分均质岩层层面顺层滑落 .因此 ,有The slip is an obvious mark in retreat of the slopes. The Fengtan Reservoir's bank is one of the slopes. It's rather shaky, and does not mean slips. The headward erosion is being cut down by the brooklets along the joints. Its headward has been stretching to the river terraces. The terrace level is being broken up; The terrace level is better than the slip when it was cut by the brooklets,but It's not slip;the deluvial eluvial is bedding plane slip at the edge of the first terrace. Therefore,the saying about the four slips is discussable.

关 键 词：滑坡 阶地 节理 溯源侵蚀 凤滩水库 库岸 稳定性 

分 类 号：TV697.23[水利工程—水利水电工程]