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降雨诱发古滑坡多期复活机制物理模拟试验研究

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雅砻江上游某拟建水电站的库区巨型滑坡近年来变形显著,对水电站的施工、运营构成严重威胁.在现场地质调查和变形分析的基础上,配制不同相似材料,采用底摩擦试验对滑坡的变形机制以及破坏模式进行研究.底摩擦试验结果表明:滑坡B1 区的后缘裂缝形成的时间较前缘裂缝的形成时间要早,裂缝规模也较大,这与现场调查、访问信息一致.B1 区监测点表明,后缘变形程度较前缘更大,符合推移式的变形模式,但若B1 区发生破坏失稳,可能造成后缘的A区局部渐进式的失稳破坏,整体上(A +B1 区)可能演化为牵引式的变形破坏模式.底摩擦试验对周家滑坡的变形破坏模式研究成果可为工程治理决策提供一定的依据.
Physical simulation experiment on multi-stage revival mechanism of ancient landslide induced by rainfall
The giant landslide in the reservoir area of a proposed hydropower station on the upper Yalong River has deformed significantly in recent years,posing a serious threat to the construction and operation of the hydropower station.On the base of on-site geologic investigation and deformation analysis,different similar materials were prepared and bottom friction test was used to study the deformation mechanism and damage mode of the landslide.The rear cracks of landslide B1 area are found to form earlier than those at the front,and their scale is also larger,as indicated by the results of bottom friction tests.This is consistented with on-site investigations and interview information.Monitoring points in B1 area indicate that the degree of rear deformation is greater than that of the front,which conforms to a translational deformation pattern.However,if instability and failure occur in B1 area,it may lead to localized progressive instability and failure in the A area of the rear.Overall(A + B1 area)may evolve into a traction-type deformation failure mode.The research results of bottom friction test on the deformation and damage mode of Zhoujia landslide can provide a certain basis for the engineering management decision.

landslidedeformation characteristicsbottom friction testresurrection deformation mechanismfailure mode

陈斌、李伟、石豫川

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雅砻江流域水电开发有限公司,成都 610051

中国电建集团华东勘测设计研究院有限公司,杭州 311100

成都理工大学 地质灾害防治与地质环境保护国家重点实验室,成都 610059

滑坡 变形特征 底摩擦试验 复活变形机制 破坏模式

国家自然科学基金

41977237

2024

水道港口
交通部天津水运工程科学研究所

水道港口

CSTPCD
影响因子:0.348
ISSN:1005-8443
年,卷(期):2024.45(1)
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