强震作用下陡倾顺层斜坡倾倒变形机制离心振动台试验
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  • 英文篇名:Centrifugal shaking table test on toppling deformation mechanism of steep bedding slope under strong earthquake
  • 作者:巨能攀 ; 邓天鑫 ; 李龙起 ; 蒋金阳 ; 张陈羊
  • 英文作者:JU Neng-pan;DENG Tian-xin;LI Long-qi;JIANG Jin-yang;ZHANG Chen-yang;State Key Laboratory of Geohazard Prevention and Geoenvironment Protection, Chengdu University of Technology;
  • 关键词:汶川地震 ; 陡倾顺层斜坡 ; 离心振动台试验 ; 动力响应 ; 失稳机制
  • 英文关键词:Wenchuan earthquake;;steep bedding slope;;centrifugal shaking table test;;dynamic response;;instability mechanism
  • 中文刊名:YTLX
  • 英文刊名:Rock and Soil Mechanics
  • 机构: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;
  • 出版日期:2018-07-12 13:45
  • 出版单位:岩土力学
  • 年:2019
  • 期:v.40;No.298
  • 基金:国家自然科学基金资助(No.41372306,No.41502299);; 成都理工大学青年骨干计划(No.KYGG201720)~~
  • 语种:中文;
  • 页:YTLX201901007
  • 页数:11
  • CN:01
  • ISSN:42-1199/O3
  • 分类号:106-115+124
摘要
陡倾顺层斜坡在静力条件下的稳定性一般较好,但是在"5.12"汶川地震中该类型斜坡却发生了大量的失稳破坏现象,通过现场调查在陡倾软硬相间顺层斜坡中发现了一类特殊的动力变形破坏模式——倾倒变形。在已有认识基础上,以四川汶川县水磨沟陡倾软硬相间顺层斜坡在强震作用下的失稳案例为基础,通过离心振动台试验研究该类型斜坡在强震作用下的倾倒变形机制和动力响应规律特性。研究表明:在斜坡表面,随着高程的增加,加速度放大系数总体表现出先增大、后减小、再增大的节律性变化,在坡高1/3处和坡肩部位动力响应呈现两个峰值。在同一水平高度下,越靠近坡表,加速度放大系数越大,即斜坡岩土体临空面效应较为显著。通过试验揭示该类斜坡失稳机制为:在强震荷载反复作用下,软岩和硬岩产生差异剪切破坏,岩土体沿优势层面下滑受阻,坡脚附近岩土体弯曲隆起,斜坡深层潜在滑面未完全贯通,坡肩震裂松弛岩体在地震的巨大水平惯性力下,向临空面作悬臂梁弯曲倾倒,整个斜坡发生拉裂滑移-下部弯曲-上部倾倒式失稳破坏。
        The stability of steep bedding slope is generally better under static force condition, but lots of instable fracture phenomena occurred in this type of slop during "5.12" Wenchuan earthquake. A special dynamic deformation failure mode, toppling deformation, is found in steep soft-hard alternative bedding slope by field investigation. Based on existing knowledge and a failure case, i.e. Shuimogou soft-hard alternative bedding of steep slope in Wenchuan County, Sichuan, the mechanism of toppling deformation and the characteristics of dynamic response of this type of slope under strong earthquake are studied by centrifugal shaking table test. On slope surface, acceleration amplification factor increases first, then decreases, and finally increases with the increase of elevation. The dynamic response shows two peak values at 1/3 of slope height and slope shoulder. At the same horizontal height, the closer to the slope surface, the greater the magnification factor of acceleration, which means that the free face effect of slope rock-soil body ismore significant. Experiment reveals the instability mechanism of this slope: under the repeated actions of strong earthquake loads,differential shear failure occurs between soft rock and hard rock, rock-soil body sliding along the dominant layer is hindered, the rock-soil body nearby slope toe bends and uplifts; the potential sliding surfaces are not connected completely, under the tremendous horizontal inertia force of earthquake, shattered rock stratum at slope shoulder generates cantilever beam bending toppling toward free face, so that the entire slope undergoes tension fracture slippage-lower bending-upper toppling instable fracture.
引文
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