喜家湾地震黄土滑坡形成机理
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  • 英文篇名:Study on the Formation Mechanism of Xijiawan Loess LandslideInduced by Earthquake
  • 作者:王明轩 ; 倪万魁
  • 英文作者:WANG Ming-xuan;NI Wan-kui;Northwest Research Institute of Engineering Investigation and Design;College of Geology Engineering and Geomatics,Chang'an University;
  • 关键词:地震滑坡 ; 形成机理 ; 黄土震陷 ; 黄土液化
  • 英文关键词:landslide induced by earthquake;;fomation mechanism;;seismic subsidence of loess;;liquefaction of loess
  • 中文刊名:HDKD
  • 英文刊名:North China Earthquake Sciences
  • 机构:西北综合勘察设计研究院;长安大学地质工程与测绘学院;
  • 出版日期:2018-02-05
  • 出版单位:华北地震科学
  • 年:2018
  • 期:v.36
  • 语种:中文;
  • 页:HDKD201801010
  • 页数:5
  • CN:01
  • ISSN:13-1102/P
  • 分类号:57-61
摘要
在喜家湾滑坡现场调查基础上,采集黄土斜坡的原状黄土和滑坡滑带土试样进行了室内试验,分析计算了滑坡土体震陷性和液化可能性;并结合滑坡发生前斜坡在地震作用下的稳定性分析及数值模拟,对该滑坡的形成机理进行了研究。研究表明,地震发生时,斜坡上部黄土产生震陷,结构破坏,下部泥岩面附近处于饱和状态的黄土在很短时间内产生了液化现象,坡体下滑形成震陷—液化复合型滑坡。
        The Xijiawan landslide,a typical loess landslide triggered by HaiYuan Earthquake in 1920 located in XiJi county was investigated in this paper.In order to clarify the formation mechanism of Xijiawan landslide,a series of tests were conducted on the loess soils collected from the main body of slope and surface of rupture in Xijiawan landslide,the possibility of seismic subsidence and liquefaction potential were analyzed,and the works of stability analysis and numerical simulation were done.The results show that the formation mechanism of landslide is the complex of seismic subsidence–liquefaction.When the earthquake happened,the destroy of seismic subsidence occurred on the upper soil of slope.Meanwhile,the saturated loess at the vicinity of lower mudstone built up loess liquefaction instantaneously.
引文
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    [3]王兰民.黄土动力学[M].北京:地震出版社,2003.
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    [5]袁中夏,王兰民,Yasuda S,等.黄土液化机理和判别标准的再研究[J].地震工程与工程振动,2004,24(4):164-169.

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