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Soil Water Characteristic Curve for a Granite Residual Soil: Experimental and Numerical Results

机译:花岗岩残留土壤的土壤水分特征曲线:实验和数值结果

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摘要

The seepage analysis in geotechnical problems, namely in excavations, was typically performed assuming saturated conditions in the ground. It is now know that the flow in the non saturated part of the ground assumes also relevant importance and hence it is vital to characterize its behaviour. The Soil Water Characteristic Curve (SWCC) of the soil is probably the most important parameter in defining this behaviour and particularly for estimating the permeability of the soil. This paper presents the definition of the SWCC for a granite residual soil using pressure plates and the filter paper method. Based on experimental data some equations are adjusted and the results obtained are discussed. At the end of the paper some predictions of the non saturated permeability of the ground are also performed.
机译:岩土工程问题(即开挖)中的渗流分析通常是在假定地下条件饱和的情况下进行的。现在知道,在地面的非饱和部分的流动也具有重要意义,因此表征其特性至关重要。土壤的土壤水分特征曲线(SWCC)可能是定义此行为的最重要参数,尤其是对于估计土壤的渗透性而言。本文介绍了使用压板和滤纸法对花岗岩残留土的SWCC的定义。根据实验数据,对一些方程进行了调整,并对所得结果进行了讨论。在本文的最后,还对地面的非饱和渗透率进行了一些预测。

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