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关于《贵州关岭“6.28”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
Issue2Pages:254-256
Other 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。
Keyword商榷 关岭滑坡 超压密岩土 边坡失稳
Subject Area环境地球化学
Indexed ByCSCD
Language中文
CSCD IDCSCD:4222559
Citation statistics
Cited Times:1[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/7051
Collection环境地球化学国家重点实验室_环境地球化学国家重点实验室_期刊论文
Recommended Citation
GB/T 7714
张信宝. 关于《贵州关岭“6.28”特大滑坡特征和成因机理》一文的商榷[J]. 山地学报,2011(2):254-256.
APA 张信宝.(2011).关于《贵州关岭“6.28”特大滑坡特征和成因机理》一文的商榷.山地学报(2),254-256.
MLA 张信宝."关于《贵州关岭“6.28”特大滑坡特征和成因机理》一文的商榷".山地学报 .2(2011):254-256.
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