强震作用下动孔隙水压力对砂质边坡动力响应的影响*
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国家高技术研究发展计划专项经费资助(2011AA11A102);铁道科学技术研究发展中心科研项目(J2014G006)


Influence of dynamic pore water pressure on dynamic response of sandy slope under strong earthquake
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    摘要:

    基于砂质边坡的弹塑性有限元模型和室内振动台试验研究了动孔隙水压力对边坡动力响应的影响规律。研究结果表明,坡脚位置的动孔隙水压力增大趋势明显,为滑坡最易剪切滑出的位置,在实际工程中应作为重点防护位置;动孔隙水压力随着平均有效应力的增加呈现总体减小的趋势;动孔压的存在使边坡在受较大动应力作用时破坏加速;由平均主应力增量引起的孔压与土的非线性变形特性无关。无地下水时,砂质边坡的坡顶首先发生拉裂破坏,表现出明显的鞭梢效应;有地下水时边坡的破坏首先出现在坡脚。地震作用下室内试验测得的动孔隙水压力整体上小于数值模拟值,但最大误差均控制在15%以内,验证了数值模拟结果的准确性。

    Abstract:

    Based on the elastic-plastic finite element model of the sandy slope and shaking table test,we study the influence laws of dynamic pore water pressure on the dynamic response.The results show that the dynamic pore water pressure of the slope toe increases obviously,and it is the destroyed position under the influence of dynamic pore water pressure,thus it should be taken as the key protection in the actual engineering location.The dynamic pore water pressure decreases with the increase of the average effective stress;The existence of dynamic pore pressure causes the destruction of the slope quickly.The pore pressure caused by the average principal stress increment has nothing to do with the nonlinear deformation characteristics of soil.Without considering the groundwater,the destruction of slope appears on the top of the slope and it shows the obvious lash effect,while the destruction appears on the slope toe.The dynamic pore water pressure values under the action of indoor test are greater than that under the numerical simulation values.However,the maximum deviation is controlled within 15% which verifies the accuracy of the numerical simulation results.

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黄 帅,吕悦军.强震作用下动孔隙水压力对砂质边坡动力响应的影响*[J].水运工程,2015(10):158-167.

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  • 在线发布日期: 2015-10-16
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