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首页> 外文期刊>Arabian journal of geosciences >Cumulative damage evolution and failure modes of the bedding rock slope under frequent microseisms
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Cumulative damage evolution and failure modes of the bedding rock slope under frequent microseisms

机译:频繁微痉挛下床上用品岩石坡的累积损伤演化与故障模式

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Most previous studies focused on the performance of bedding rock slope under strong earthquakes, where limited publications involved bedding rock slope under microseisms. Present literatures often ignored the effect of rock joint surface shapes on slope stability and just simplified it as a planar surface, which is always not practical. In this study, shaking table test was carried out to study the dynamic behavior, damage accumulation, and failure mode of the bedding rock slope with zigzag asperities under frequent microseisms. Generally, the natural frequency decreases with the increase of loading times of earthquakes, while the damping ratio of the slope has a tendency to grow with it. Results shows that the main failure mode of model slope was integral slipping along the bedding surface, and two sliding surfaces were observed during the instability evolution process of the model slope, indicating that the deformation pattern of the sliding surface was mostly determined by undulating angles and normal stress. Besides, the cumulative damage of the slope was evaluated based on the variation of natural frequency, and the cumulative damage evolution models of slope rock mass were established respectively for stages of micro-small earthquakes and strong earthquakes. It is found that the evolution curve of cumulative damage was characterized by a tendency of slight decline to rapid growth to steady growth under micro-small earthquakes, while it followed an exponential growth trend under strong earthquakes.
机译:最先前的研究侧重于强大地震下床上用品岩石坡的性能,其中有限的出版物涉及微血症下的床上用品岩石坡。目前的文献通常忽略了岩石接头表面形状对斜坡稳定性的影响,并且简化为平面表面,这总是不实用的。在这项研究中,进行了摇动台测试,以研究床上用品的动态行为,损坏和失效模式与频繁微痉挛的曲折粗糙。通常,随着地震装载时间的增加,自然频率降低,而斜坡的阻尼比率随之生长而来。结果表明,在模型斜率的不稳定演变过程中,模型斜面的主体故障模式是沿床上表面的整体滑动,并且在模型斜率的不稳定演变过程中观察到两个滑动表面,表明滑动表面的变形图案主要通过起伏的角度确定正常压力。此外,基于自然频率的变化评估了斜坡的累积损伤,分别为微小地震和强烈地震阶段建立了坡岩体的累积损伤演化模型。结果发现,累积损伤的演化曲线的特征在于微小地震下稳定增长略微下降的趋势,而在强烈地震下,它遵循指数增长趋势。

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