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某水电站坝前左岸高边坡深部破裂形成机制分析
引用本文:严明,黄润秋,徐佩华. 某水电站坝前左岸高边坡深部破裂形成机制分析[J]. 成都理工大学学报(自然科学版), 2005, 32(6): 609-613
作者姓名:严明  黄润秋  徐佩华
作者单位:成都理工大学"地质灾害防治与地质环境保护"国家专业实验室,成都,610059;吉林大学建设工程学院,长春,130026
摘    要:某拟建水电站坝前左岸反倾边坡,除正常卸荷裂隙外,在坡体深处发育一系列变形破裂迹象.对其成因分析研究表明,这套深部破裂是处于高地应力环境的反倾边坡,在河谷快速下切过程中,发生深部卸荷松弛所致,属于一种稳定的变形破裂结构.这一认识有助于正确评价坝前左岸边坡稳定性.

关 键 词:反倾边坡  深部破裂  卸荷  倾倒
文章编号:1671-9727(2005)06-0609-05
收稿时间:2005-03-08
修稿时间:2005-03-08

Research on the deep-seated deformation mechanism of the left bank slope in the front of a dam, Sichuan, China
YAN Ming,HUANG Run-qiu,XU Pei-hua. Research on the deep-seated deformation mechanism of the left bank slope in the front of a dam, Sichuan, China[J]. Journal of Chengdu University of Technology: Sci & Technol Ed, 2005, 32(6): 609-613
Authors:YAN Ming  HUANG Run-qiu  XU Pei-hua
Affiliation:1. National Laboratory of Geo-hazard Prevention and Geo-environment Protection, Chengdu University of Technology, Chengdu 610059, China; 2. College of Construction Engineering, J iling University, Changchun 130026, China
Abstract:The geologic exploration shows that except the normal relaxed cracks,there exists a kind of deep-seated deformation-fracture system inside the left bank slope in the front of a dam.The genesis of the fracture system is studied in this paper.It can be concluded that the fracture system observed in the high slope,being reverse and in a high-intensive geo-stress environment,is caused by the stress release during the rapid down-cutting of the river.Therefore,this fracture system is a stable structure.This conclusion will be conducive to the evaluation of the high slope stability.
Keywords:reverse slope  deep-seated fracture  relaxation  toppling  
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