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Assessment of the behaviour of soil structure in double-porosity kaolin media using light transmission visualization (LTV) method

机译:用光透射可视化(LTV)方法评估双孔隙高岭土介质中土壤结构的行为

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摘要

Double-porosity is a phenomenon that occurs naturally and can be found in many subsurface media such as rock aquifers, agricultural topsoils and compacted soils. These media have different pore size characteristics that result in different hydraulic properties. Two approaches were used to create the double-porosity soil structure using kaolin clay to be tested in migration of contaminant experiments using light transmission visualization (LTV) method. Aggregated kaolin and sintered clayey spheres mixture were used as the media for the first and second test, respectively. The observation shows that the first approach is not viable for a saturated-porous medium because kaolin particles have disintegrated and turned into emulsion. In contrast, uniform kaolin particles that remain strong and solid have been produced using the second approach. In conclusion, the LTV method is viable to monitor the behaviour of fluids in porous media under different conditions.
机译:双孔隙现象是自然发生的现象,可以在许多地下介质中找到,例如岩石含水层,农业表层土壤和压实土壤。这些介质具有不同的孔径特征,从而导致不同的水力特性。两种方法被用来使用高岭土创建双孔隙土壤结构,并使用光透射可视化(LTV)方法在污染物迁移实验中进行测试。聚集的高岭土和烧结的粘土球混合物分别用作第一和第二测试的介质。观察结果表明,第一种方法不适用于饱和多孔介质,因为高岭土颗粒已经分解并变成乳液。相反,使用第二种方法已经制得了保持坚固和固体的均匀高岭土颗粒。总之,LTV方法在不同条件下监测多孔介质中流体的行为是可行的。

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