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Prediction of silt soil subgrade moisture content based on unsaturated seepage theory

机译:基于非饱和渗流理论的粉砂土路基含水量预测

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In order to study the distribution of water in silt soil subgrade, this paper establish finite element model based on unsaturated seepage theory to research the groundwater level, rainfall, evaporation factors influencing on the moisture content of subgrade and side slope materials. The results show that: the moisture content of suhbgrade exponential growth with the water table. Continuous evaporation or rainfall influence the subgrade slope with the depth of 0.2–0.6m; finite element model based on unsaturated seepage theory can predict the water content in subgrade accurately and meet the project construction need.
机译:为了研究粉砂土路基中水的分布,建立了基于非饱和渗流理论的有限元模型,研究了地下水位,降雨,蒸发因子对路基和边坡材料含水量的影响。结果表明:水位与地下水的指数增长呈负相关。连续的蒸发或降雨会影响路基边坡,深度为0.2-0.6m。基于非饱和渗流理论的有限元模型可以准确预测路基中的含水量,满足工程建设的需要。

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