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地震作用下含软弱夹层的反倾向岩质边坡动力响应及变形破坏机制研究

ynamic response and deformation and failure mechanism of a toppling rock slope under earthquakes

中文摘要英文摘要

本文建立了一含软弱夹层的反倾岩质边坡三维模型,运用有限差分软件FLAC3D,首先对其在地震作用下的加速度响应规律进行了研究,然后通过对该边坡塑性区的性质、形成次序、扩展情况、软弱夹层内关键单元剪应变增量的变化研究分析了其变形机制。结果表明:地震作用下含软弱夹层的反倾岩质边坡坡面点水平向和垂向加速度峰值放大系数随高程增加均呈增大趋势;岩体对输入地震波存在垂直放大作用,在软弱夹层处和坡顶增幅较大。岩体对地震波低频段的能量起到放大作用,对高频段的地震波存在滤波作用,但滤波作用并不明显;反倾岩质边坡变形破坏主要发生在软弱夹层中,塑性区表现为在软弱夹层上部拉破坏与下部拉剪破坏。

his article Established a three-dimensional model of the toppling rock slope with weak layer, First The acceleration response regulation of a toppling rock slope under the seismic action is discussed by using the three-dimensional finite difference software FLAC3D. Then the deformation and failure mechanism is analyzed through the nature of the plastic zone, the formation of order, the expansion of the plastic zone, changes of shear strain increment of key elements , The results showed that: under the seismic action, the amplification coefficients of the horizontal and vertical peak accelerations of the toppling rock slopes increase with the increasing elevation. The rock mass has vertical amplification effect on the input seismic waves and come to the maximum at the weak layer and the top of the slope. And the effect amplified the input seismic waves with low frequency and filtered those with high frequency.But the filtering effect is not obvious; toppling rock slope deformation and failure occurs mainly in the weak layer, The performance of the plastic zone is the upper tensile failure and the lower part of the pull-shear failure with weak layer.

黄云飞、谌文武、邵东桥

地质学

反倾岩质边坡软弱夹层地震作用动力响应变形机制

oppling rock slopeweak interlayerearthquakedynamic responsedeformation mechanism

黄云飞,谌文武,邵东桥.地震作用下含软弱夹层的反倾向岩质边坡动力响应及变形破坏机制研究[EB/OL].(2013-03-08)[2025-08-02].http://www.paper.edu.cn/releasepaper/content/201303-340.点此复制

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