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The Influence of Some Chemical Properties of Soaking Liquids on the Collapse of Tropical Soils

机译:浸泡液的某些化学性质对热带土壤崩塌的影响

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Soil structure depends on many variables in the system particles and surrounding soil water, thus it is reasonable to suppose that the magnitude of soil collapse strain can vary, under certain use conditions, like following sewer and different chemical effluent leakage. This paper deals with the influence of liquids of various compositions and chemical properties on the collapse behavior of two typical tropical soils, considering the magnitude of collapse strain, its development over time, and the variation in soil porosity as a result of the volumetric reduction after soil collapse. The paper shows that the pH of liquids is related to soil collapse to a limited extent, as is the case for organic liquids and sodium hydroxide solutions used in this study. However, pH is not an efficient unifying property in indicating the magnitude of soil collapse. Collapse strain also increases with the dielectric constant of the organic liquids used in the tests. Soil collapse strain reduces the amount and diameter of soil macropores, modifying soil pore distribution.
机译:土壤结构取决于系统颗粒和周围土壤水的许多变量,因此可以合理地假设在某些使用条件下,例如下水道和不同的化学废水泄漏,土壤塌陷应变的大小可以变化。本文考虑了各种不同组成和化学性质的液体对两种典型热带土壤坍塌行为的影响,其中考虑了塌陷应变的大小,其随时间的发展以及土壤体积减少后土壤孔隙度的变化。土壤塌陷。论文表明,液体的pH值在一定程度上与土壤崩塌有关,本研究中使用的有机液体和氢氧化钠溶液也是如此。但是,pH值不是指示土壤崩塌程度的有效统一属性。塌陷应变也随着测试中使用的有机液体的介电常数而增加。土壤塌陷应变减少了土壤大孔的数量和直径,改变了土壤的孔隙分布。

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