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Experimental Investigation of the Effects of Suffusion on Physical and Geomechanic Characteristics of Sandy Soils

机译:灌水对沙质土壤物理力学特性的影响的实验研究

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This paper reports the measured effects of suffusion, a type of internal erosion, on the physical and geo-mechanical properties of soils including permeability, volume change, compressive strength, and soil grains gradation. A poorly graded river sand with the addition of 10 % kaolinite clay was used to create three gap-graded soils and an unaltered poorly graded "original soil." Testing was performed using a modified triaxial apparatus that permits seepage through compacted specimens and allows collection of effluent and eroded soils. The specimens, 5.1 cm in diameter and 10.2 cm in length, were monitored for changes in volume and permeability during the suffusion tests. After erosion, the specimens were compressed using the consolidated-undrained (CU) test. The collected effluent samples were dried to determine the erosion rate and eroded soil particle gradations with respect to effluent volume. Companion control specimens were tested without erosion. The results revealed that suffusion may affect some physical and geo-mechanical properties of soils. Permeability reduction was generally observed in all soils, indicating fine grains migration and clogging within the specimens. The three gap-graded soils each exhibited a greater degree of internal erosion (suffusion), permeability reduction, and volume change than the original soil. The experimental setup and testing protocol also provided a feasible methodology for further research on the effects of suffusion on the physical and geo-mechanical properties of soils. Limitations of this research and future research recommendations on this topic are provided at the end of this paper.
机译:这篇论文报道了内部侵蚀类型的灌水对土壤物理和地质力学特性(包括渗透率,体积变化,抗压强度和土壤颗粒分级)的测量影响。使用等级差的河砂和10%的高岭石粘土来创建三种间隙等级的土壤和未更改的等级差的“原始土壤”。使用改良的三轴仪器进行测试,该仪器允许渗入压实的样品并允许收集污水和侵蚀土壤。在注液测试期间,对直径为5.1厘米,长度为10.2厘米的样品进行体积和渗透率监测。腐蚀后,使用固结排水(CU)试验压缩样品。干燥收集的污水样品,以确定相对于污水量的侵蚀率和侵蚀的土壤颗粒等级。对同伴对照样品进行了测试,没有腐蚀。结果表明,灌水可能会影响土壤的某些物理和地质力学特性。通常在所有土壤中都观察到渗透率降低,这表明细颗粒迁移并在样品内发生堵塞。与原始土壤相比,三种间隙分级的土壤均表现出更大程度的内部侵蚀(富集),渗透率降低和体积变化。实验设置和测试方案还为进一步研究灌流对土壤物理和地质力学特性的影响提供了可行的方法。本文的最后提供了该研究的局限性以及有关该主题的未来研究建议。

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