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张良以, 陈铁林, 张顶立. 降雨诱发膨胀土边坡渐进破坏研究[J]. 岩土工程学报, 2019, 41(1): 70-77. DOI: 10.11779/CJGE201901007
引用本文: 张良以, 陈铁林, 张顶立. 降雨诱发膨胀土边坡渐进破坏研究[J]. 岩土工程学报, 2019, 41(1): 70-77. DOI: 10.11779/CJGE201901007
ZHANG Liang-yi, CHEN Tie-lin, ZHANG Ding-li. Progressive failure of expansive soil slopes under rainfall[J]. Chinese Journal of Geotechnical Engineering, 2019, 41(1): 70-77. DOI: 10.11779/CJGE201901007
Citation: ZHANG Liang-yi, CHEN Tie-lin, ZHANG Ding-li. Progressive failure of expansive soil slopes under rainfall[J]. Chinese Journal of Geotechnical Engineering, 2019, 41(1): 70-77. DOI: 10.11779/CJGE201901007

降雨诱发膨胀土边坡渐进破坏研究

Progressive failure of expansive soil slopes under rainfall

  • 摘要: 膨胀变形是膨胀土边坡失稳破坏的重要因素之一,研究分析降雨诱发膨胀土边坡渐进破坏过程具有重要的实践意义。基于膨胀应变与基质吸力增量的线性关系,将膨胀性引入非饱和流固耦合模型当中,建立一种适用于膨胀土工程的非饱和渗流场-应力场-膨胀应变场多场耦合数值计算方法。结合应变软化模型,分析单次降雨诱发下膨胀土边坡入渗过程以及边坡渐进破坏全过程。结果表明,非饱和膨胀土边坡在单次降雨诱发后,坡体发生以坡脚为起始逐渐向坡顶扩展的破坏,具有明显的时间延后性、多层逐级后退式的特点。膨胀土的膨胀性、强度参数对坡体破坏形式具有显著的影响,膨胀土边坡破坏既保留了一般黏性土的共性也呈现出干缩湿胀的特殊性。

     

    Abstract: The expansive deformation caused by rainfall is one of important factors for the failure of expansive soil slopes. Therefore, it is of great practical significance to analyze the progressive failure process of expansive soil slopes under rainfall. Based on the linear relationship between expansion strain and matrix suction increment, a numerical analysis method for multi-field coupling of unsaturated seepage, stress and expansion strain fields is proposed. Based on the strain-softening model, the infiltration process of an expansive soil slope induced by single rainfall and the complete process of its progressive failure are presented. The results show that the progressive failure of the unsaturated expansive soil slope occurs at the foot of the slope and extends gradually to the top. It has the characteristics of time delay, multistage and retrogression. The expansive and strength parameters of expansive soils have significant influences on the failure form of the slope. The failure of expansive soil slopes retains the commonness of the general cohesive soils and presents the particularity of dry shrinkage and wet expansion.

     

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