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Laboratory investigation of the effect of cyclic wetting and drying on the behaviour of an expansive soil

机译:循环润湿和干燥对膨胀土性能影响的实验室研究

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摘要

The behaviour of an expansive soil was studied through a number of experiments involving cycles of wetting and drying. Laboratory tests were conducted on compacted samples of an expansive soil (a mixture of bentonite and kaolin, CH) in a modified oedometer under different constant surcharge pressures. The Void ratio and water content of samples were determined at different stages. The results show that the swelling shrinkage was reversible after the soil reached the equilibrium condition where the deformations were the same and the wetting and drying paths (in the water content void ratio space) converged to an S-shaped curve. The hysteresis phenomenon was studied through the variation of the void ratio with suction, and the results showed that it diminished gradually with the increase in cycles of wetting and drying. The effect of fabric on the behaviour of soil samples was studied during cycles of wetting and drying. The results show that the samples with lower initial water content (on the dry side of optimum) have more swelling potential than samples with a higher initial water content (on the wet side of optimum). (C) 2015 The Japanese Geotechnical Society. Production and hosting by Elsevier B.V. All rights reserved.
机译:通过一系列涉及润湿和干燥循环的实验研究了膨胀土的行为。在改良的里程表中,在不同的恒定附加压力下,对膨胀土(膨润土和高岭土的混合物,CH)的压实样品进行了实验室测试。在不同阶段确定样品的空隙率和水含量。结果表明,当土壤达到变形相同的平衡条件后,其干缩路径是可逆的,并且干湿路径(在含水率空隙率空间中)收敛为S形曲线。通过空洞率随吸力的变化研究了磁滞现象,结果表明,随着润湿和干燥周期的增加,磁滞现象逐渐减小。在润湿和干燥的循环过程中,研究了织物对土壤样品行为的影响。结果表明,初始水含量较低(最佳状态的干燥)的样品比初始水含量较高(最佳状态的潮湿)的样品具有更大的溶胀潜力。 (C)2015年日本岩土学会。 Elsevier B.V制作和托管。保留所有权利。

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