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首页> 外文期刊>Soils and foundations >A CASE STUDY ON THE IN-SITU MATRIX SUCTION MONITORING AND UNDISTURBED-SAMPLE LABORATORY TEST FOR THE UNSATURATED COLLUVIUM SLOPE
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A CASE STUDY ON THE IN-SITU MATRIX SUCTION MONITORING AND UNDISTURBED-SAMPLE LABORATORY TEST FOR THE UNSATURATED COLLUVIUM SLOPE

机译:非饱和岩质边坡原位基质吸力监测和无扰动实验室试验的案例研究

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摘要

References(18) Cited-By(3) Huafan University is located on the slope of the Ta-Lun Mountain area. The slope surface in this area is a colluvium soil cover layer with loose non-uniform particles, with high permeability. Because it is situated above a rapidly changing water table, the pore water pressure varies dynamically, depending on the weather conditions. In the dry season, most of the topsoil behaves in the unsaturated condition such that the matrix suction in the soil increases its shearing strength. In contrast, when heavy rainfall occurs, the seepage by precipitation tends to destroy the existing matrix suction. This reduction in soil strength frequently results in slope failure. This study, focuses on the variation of matrix suction of the colluvium soil in different precipitation conditions with varying vegetation at the campus of Huafan University. The analysis of the in-situ monitoring results and the laboratory test results for the undisturbed specimens taken from the field, with shearing strength and matrix suction taken into account. It is expected the results to be a useful reference for disaster protection on slopes.
机译:参考文献(18)被引用的华范大学(3)位于塔伦山区的斜坡上。该区域的坡面是具有松散不均匀颗粒,高渗透性的集积土壤覆盖层。由于它位于快速变化的地下水位上方,因此孔隙水压力会根据天气情况动态变化。在干旱季节,大多数表层土表现为非饱和状态,因此土壤中的基质吸力增加了其剪切强度。相反,当出现强降雨时,降水造成的渗流倾向于破坏现有的基质吸力。土壤强度的这种降低经常导致边坡破坏。本研究着重研究了华帆大学校园内不同降水条件下不同植被下坡地土壤基质吸力的变化。考虑到抗剪强度和基质吸力,对现场采集的未受干扰样品的现场监测结果和实验室测试结果进行了分析。预期结果将为斜坡的防灾工作提供有用的参考。

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