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

机译:浸泡液体对热带土壤塌陷的影响对热带土壤的影响

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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中的许多变量,因此假设土壤塌陷菌株的大小可以在某些使用条件下变化,如下水道和不同的化学出水泄漏。本文涉及各种组合物和化学性质液体对两个典型的热带土壤的塌陷行为的影响,考虑到坍塌菌株的大小,随着时间的推移,其开发和土壤孔隙率的变化土壤崩溃。本文表明,液体pH与有限程度的土壤塌陷有关,本研究中使用的有机液体和氢氧化钠溶液的情况如此。然而,pH不是一种有效的统一性,表明土壤崩溃的幅度。折叠应变也随测试中使用的有机液体的介电常数增加。土壤塌陷菌株降低土壤大孔的量和直径,改性土壤孔隙分布。

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