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An experimental testing apparatus for study of suffusion of granular soils in geological structures

机译:用于研究地质结构中粒状土壤弥散性的实验测试设备

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摘要

This study mainly focuses on the suffusion process of granular soils, especially that filled in geological structures, such as faults and karst conduits. As current devices only can be used for suffusion tests on cylindrical soil specimens, an experimental testing apparatus has been designed and developed for systematic research on the suffusion of granular soils filled in fractures and fractures subjected to unidirectional seepage flow. The permeameter cell is designed to enable free rotation so that unidirectional seepage can be imposed at any angle from 0 degrees to 90 degrees. Experiments on granular soils were carried out under different axial stresses to verify the operability and repeatability of the designed apparatus. The water pressure and axial stress applied on soil specimens were controlled during testing, and the variations of flow rate and hydraulic conductivity with water pressure under different axial stresses were analyzed to study the effect of axial stress on the suffusion of granular soils.
机译:这项研究主要关注粒状土壤的注水过程,尤其是充填在诸如断层和岩溶导管等地质结构中的土壤。由于目前的设备只能用于圆柱土壤标本的注水试验,因此设计并开发了一种实验测试设备,用于系统研究填充在裂缝和单向渗流中的裂缝中的粒状土壤的注水。渗透计池设计为可自由旋转,因此可以在0度到90度之间的任意角度施加单向渗流。在不同的轴向应力下对粒状土壤进行了实验,以验证所设计设备的可操作性和可重复性。在试验过程中控制施加在土壤标本上的水压力和轴向应力,并分析了在不同轴向应力下流量和水力传导率随水压的变化,以研究轴向应力对粒状土壤团聚的影响。

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