IMHE OpenIR  > 山地表生过程与生态调控重点实验室
关于贵州关岭628特大滑坡特征和成因机理一文的商榷
张信宝
2011
Source Publication山地学报
ISSN1008-2786
Volume029Issue:002Pages:254
Abstract就滑坡组成和发生机制,与《贵州关岭"6.28"特大滑坡特征和成因机理》一文作者进行商榷。笔者认为"超压密岩土边坡失稳理论"可以较好的解释大寨滑坡-碎屑流灾害的突然发生。"上硬下软"坡体结构,是大寨滑坡发生的地质基础;强降雨快速入渗,是导致岩层裂隙和大气突然贯通,负压立即消失,高陡坡体迅即失稳的诱因。
Language英语
Document Type期刊论文
Identifierhttp://ir.imde.ac.cn/handle/131551/31603
Collection山地表生过程与生态调控重点实验室
Affiliation中国科学院成都山地灾害与环境科学研究所
First Author Affilication中国科学院水利部成都山地灾害与环境研究所
Recommended Citation
GB/T 7714
张信宝. 关于贵州关岭628特大滑坡特征和成因机理一文的商榷[J]. 山地学报,2011,029(002):254.
APA 张信宝.(2011).关于贵州关岭628特大滑坡特征和成因机理一文的商榷.山地学报,029(002),254.
MLA 张信宝."关于贵州关岭628特大滑坡特征和成因机理一文的商榷".山地学报 029.002(2011):254.
Files in This Item:
There are no files associated with this item.
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[张信宝]'s Articles
Baidu academic
Similar articles in Baidu academic
[张信宝]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[张信宝]'s Articles
Terms of Use
No data!
Social Bookmark/Share
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.