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Analysis of Soil Structures and the Mechanisms under the Action of Freezing and Thawing Cycles

机译:冻融循环作用下的土壤结构及机理分析

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A series of indoor tests were conducted to study the changes of soil particles and pores under freezing and thawing cycles. Testing results showed that grain breakages of coarse particles occurred during freezing and thawing cycles, resulting in an increase of the Atterberg limits and specific surface area of the soil samples. Meanwhile, the pore size distribution, tested by the mercury intrusion method, was also changed during the cycles; macro pores increased, mini pores reduced, and micro pores remained roughly unchanged. The interaction of soil particles (solid phase), soil pores (gas phase), and soil water (liquid phase), namely soil's three phase components, is discussed to explore the change mechanisms of soil structures under freezing and thawing cycles.
机译:进行了一系列室内试验,研究了冻融循环下土壤颗粒和孔隙的变化。测试结果表明,在冷冻和解冻过程中,粗颗粒会发生颗粒破裂,从而导致阿特伯格极限值和土壤样品的比表面积增加。同时,通过水银压入法测试的孔径分布在循环过程中也发生了变化。大孔增加,小孔减少,微孔大致保持不变。讨论了土壤颗粒(固相),土壤孔隙(气相)和土壤水(液相)(即土壤的三相成分)之间的相互作用,探讨了土壤结构在冻融循环下的变化机理。

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