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Effect of Fines on Hysteretic Hydraulic Conductivity of Unsaturated Soil

机译:细粉对非饱和土滞回水力传导率的影响

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Soil cover systems such as capillary barriers and compacted covers experience cyclic drying and wetting induced by evaporation and infiltration. These wetting and drying cycles have hysteretic effect on hydraulic properties of unsaturated soils. Numerous studies on hysteresis in soil water characteristic curve (SWCC) have been reported in the literature but only a limited number of studies deal with hysteretic unsaturated permeability of compacted sand-clay mixtures. In the present study, a series of laboratory permeability tests have been carried out to investigate the effect of fines on hysteretic hydraulic conductivity of unsaturated soil. The coefficient of unsaturated hydraulic conductivity of sand-kaolin mixtures containing 0%, 10%, and 30% kaolin by dry weight was detennined for both drying and wetting cycles. A modified triaxial apparatus was used to apply suction and hydraulic head to measure the unsaturated permeability at different values of matric suction. Test results show that the hysteresis effect on permeability increases considerably with an increase in fines content in sand-clay mixtures.
机译:土壤覆盖系统(例如毛细屏障和压实的覆盖物)会经历因蒸发和渗透而引起的周期性干燥和湿润。这些润湿和干燥循环对非饱和土壤的水力特性具有滞后作用。文献中已经对土壤水分特征曲线(SWCC)中的滞后现象进行了大量研究,但只有少数研究涉及压实砂土混合物的滞后性不饱和渗透率。在本研究中,已经进行了一系列的实验室渗透性试验,以研究细粉对非饱和土的滞回水力传导率的影响。确定干重为0%,10%和30%的高岭土砂土混合物的不饱和水导率系数,用于干燥和润湿循环。使用改进的三轴仪器施加吸力和液压压头,以测量不同基质吸力值下的非饱和渗透率。测试结果表明,随着砂土混合物中细粉含量的增加,磁滞效应对磁导率的影响也显着增加。

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