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陈勇, 王世梅, 刘德富, 田东方. 三维非饱和土滑坡稳定性影响因素研究[J]. 岩土工程学报, 2010, 32(8).
引用本文: 陈勇, 王世梅, 刘德富, 田东方. 三维非饱和土滑坡稳定性影响因素研究[J]. 岩土工程学报, 2010, 32(8).
Factors for stability of three-dimensional unsaturated soil landslides[J]. Chinese Journal of Geotechnical Engineering, 2010, 32(8).
Citation: Factors for stability of three-dimensional unsaturated soil landslides[J]. Chinese Journal of Geotechnical Engineering, 2010, 32(8).

三维非饱和土滑坡稳定性影响因素研究

Factors for stability of three-dimensional unsaturated soil landslides

  • 摘要: 三维空间结构和土体非饱和状态,对滑坡稳定性评价具有至关重要的影响。为了深入研究影响三维非饱和土滑坡稳定性的主要因素,以标准算例的三维扩展模型为例,考虑非饱和土的弹塑性本构模型和Fredlund强度准则,开展边坡稳定性数值模拟研究。从外因和内因两个方面,探讨了雨水入渗引起的负孔隙水压力分布和地下水位线的改变以及滑面深度、强度参数等因素对三维非饱和土滑坡稳定性的影响规律。研究结果表明:采用三维分析方法能反映坡体的空间应力状态和滑面的空间形态,各分析因素对滑坡稳定性的影响程度依次为参数 的改变、雨水入渗导致吸力丧失、滑面深度,且 的影响随着滑面深度而增大,而雨水入渗对浅层滑坡的影响较大。

     

    Abstract: Three-dimensional structure and unsaturated condition have essential influences on the evaluation of slope stability. In order to study the main influencing factors on the stability of unsaturated soil slopes, an extended three-dimensional model for standard tests is taken as the example, then based on elasto-plastic constitutive model and strength criterion of unsaturated soils, the numerical simulations of slope stability are carried out. From the two aspects of external and internal factors, the influencing rules on the stability of three-dimensional unsaturated soil slopes are analyzed by discussing the variation of negative pore water pressure distribution and underground water table caused by rainwater infiltration as well as the depth of sliding surface and the strength parameters. The results show that the three-dimensional method can reflect the spacial stress state and the shape of sliding surface, and that the influence degree of each analytical factors on the slope stability is successively the variation of , the decline of suction due to water infiltration and the depth of sliding surface. With the depth increase, the effect of increases, and the water infiltration has obvious influences on the shallow landslides.

     

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