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Infiltration Characteristics of Granite Cover Soil Considering Unsaturated Condition

机译:考虑不饱和条件的花岗岩覆盖土的渗透特性

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Infiltration characteristics of Shinae-dong granite soil considering unsaturated condition were investigated in this study. Laboratory tests and statistics analyses were undertaken to examine the effect of relative compaction and water content on the soil-water characteristic curve. The soil-water characteristic curves for Shinnae-dong soil varies with relative compaction of soils, but initial water content seems not to affect the soil-water characteristic curve significantly. Laboratory column tests were conducted for various relative compactions, and the results of the test were simulated using the finite difference analysis. Parameters used for numerical analysis were estimated from the results of laboratory tests. The specimen with low relative compaction requires less time to saturate the full depth than that with high relative compaction.
机译:研究了考虑不饱和条件的Shinae-Dong花岗岩土壤的渗透特性。进行了实验室测试和统计分析,以研究相对压实和水含量对土壤 - 水特征曲线的影响。 Shinnae-Dong土壤的土壤 - 水特征曲线随着土壤的相对压实而变化,但初始水含量似乎不会显着影响土壤 - 水特征曲线。进行实验室柱试验,进行各种相对保,并使用有限差分分析模拟测试结果。从实验室测试的结果估计了用于数值分析的参数。具有低相对压实的标本需要较少的时间来使完全深度饱和而不是高相对压实。

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