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Effects of Suction Path on Water Retention and Volumetric Behavior of Loess at High Suctions

机译:吸入路径对高吸水下黄土水保留和体积行为的影响

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This study aims to investigate the effects of suction path, i.e., drying or wetting, on water retention curve (WRC) and volume changes of intact and re-compacted loess. Two series of WRC tests were carried out in which soil specimens were subjected to two different suction paths, namely: WD (wetting to saturation from the initial state followed by drying and wetting) and DW (drying from the initial state followed by wetting). Vapor transfer technique was used to control suction in the range of 4-290 MPa. Experimental results revealed that WRCs of intact and re-compacted loess are not significantly affected by suction path within the studied suction range in which adsorption of water is dominant in controlling water retention compared with the pore structure. However, volume changes are observed to be path dependent because of the collapse of loess structure caused in the WD path but not in the other one.
机译:本研究旨在探讨吸力路径,即干燥或润湿,水保留曲线(WRC)和完整和重新压实黄土的体积变化的影响。进行了两种系列的WRC测试,其中土壤样品经受两种不同的吸入路径,即:WD(从初始状态润湿,然后干燥和润湿)和DW(从初始状态干燥,然后润湿)。蒸汽转移技术用于控制4-290MPa范围内的吸力。实验结果表明,完整和重新压实黄土的WRC没有显着影响所研究的吸入范围内的吸入路径,其中水吸附在与孔结构相比的控制水保留方面是显性的。然而,由于在WD路径中引起的黄土结构崩溃但不在另一个,因此观察到卷的变化是依赖的。

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