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A PRACTICAL NUMERICAL MODEL FOR SEEPAGE BEHAVIOR OF UNSATURATED SOIL

机译:非饱和土渗流特性的实用数值模型

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References(9) Cited-By(4) It is important to estimate the seepage properties of unsaturated soils when performing an unsaturated-saturated seepage analysis, which is used to clarify the slope failure mechanism and predict the occurrence time of slope failure due to rainfall. Kitamura et al. (1998) proposed a numerical model to quantitatively estimating the seepage properties of unsaturated soils. And they have compared numerical results with laboratory soil tests in order to examine the validity of the numerical model. Consequently, it has been found that the numerical model must be improved moreover. In this paper a practical numerical model for seepage behavior of unsaturated soil is proposed to improve the previous model proposed by Kitamura et al. (1998). Firstly, the basic theories of the previous model are explained. Calculation results are compared with those obtained from the laboratory soil tests in order to examine the validity of the previous model. Then, we perform some improvements of the previous model based on hydro-mechanical properties, and propose a new parameter, named “parallel translation index (Ipt)”. From the results we showed that the relationship between the new parameter and the uniformity coefficient (Uc), expressed by logarithm is linear relation. Therefore, the reasonable seepage properties of soils can be computed from the improved numerical model using only the popular soil parameters.
机译:参考文献(9)By-By(4)在进行非饱和-饱和渗流分析时,估算非饱和土壤的渗透性很重要,它可用于阐明边坡破坏机理并预测降雨引起的边坡破坏发生时间。 。北村等。 (1998)提出了一个数值模型来定量估计非饱和土的渗透性。他们将数值结果与实验室土壤测试进行了比较,以检验数值模型的有效性。因此,已经发现,还必须改进数值模型。本文提出了一种实用的非饱和土渗透性数值模型,以改进Kitamura等人提出的先前模型。 (1998)。首先,说明先前模型的基本理论。为了验证先前模型的有效性,将计算结果与从实验室土壤测试获得的结果进行比较。然后,我们基于流体力学特性对先前模型进行了一些改进,并提出了一个新参数,称为“平行平移指数(Ipt)”。从结果可以看出,新参数与均匀性系数(Uc)之间的关系以对数表示为线性关系。因此,仅使用常用的土壤参数,就可以从改进的数值模型中计算出合理的土壤渗透性。

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