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Thermal effects on water retention behaviour of unsaturated collapsible loess

机译:不饱和折叠黄土水保留行为的热效应

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Purpose Temperature has a significant influence on water retention curve (WRC) because temperature affects surface tension of water and volumetric behaviour of soil. However, in previous studies on thermal effects on WRC, the difference in suction-induced volume change of soil specimen at various temperatures is always insignificant. With increasing temperature, the wetting-induced collapse of loess increases. This study aims to investigate thermal effects on WRC of collapsible loess. Material and methods A loess from Shaanxi province, China, is tested. Wetting-drying tests were carried out on compacted loess specimens at temperatures ranging from 5 to 50 degrees C. Thermal effects on water retention behaviour of collapsible loess are analysed. Results and discussion During the wetting process, volumetric water content at a given suction at 50 degrees C is 20% smaller than that at 5 degrees C. This is because when temperature increases from 5 to 50 degrees C, surface tension of water decreases by 10% and wetting-induced volumetric contraction increases by three times. During drying, the air entry value (AEV) of loess decreases with increasing temperature at a rate of 0.16%/degrees C. Conclusions The retention capability of unsaturated loess decreases with increasing temperature. For the tested collapsible loess, with increasing temperature, a combined effect of smaller water surface tension and larger wetting-induced collapse results in a prominent decrease in volumetric water content of loess. Moreover, the decrease of AEV induced by smaller surface tension is partially compensated by effects of larger wetting-induced collapse on AEV.
机译:目的温度对水保持曲线(WRC)产生了显着影响,因为温度影响水的表面张力和土壤的体积行为。然而,在先前关于WRC的热效应的研究中,在各种温度下土壤样品的吸入诱导体积变化的差异总是微不足道的。随着温度的增加,润湿引起的黄土坍塌增加。本研究旨在调查对可折叠黄土无线的热效应。材料和方法中国陕西省的黄土进行了测试。在压实的黄土标本下在5至50摄氏度的温度下进行润湿干燥试验。分析了可折叠黄土水保留行为的热效应。结果与讨论在润湿过程中,50℃的给定抽吸的体积水含量比5摄氏度小20%。这是因为当温度从5到50℃增加时,水的表面张力减少10 %和润湿诱导的体积收缩增加了三次。在干燥过程中,黄土的空气入口值(AEV)随着0.16%/℃的速率的增加而降低。结论不饱和黄土的保留能力随温度的增加而降低。对于测试的可折叠黄土,随着温度的增加,较小的水表面张力和较大的润湿引起的塌陷的组合效果导致黄土体积含水量的突出减少。此外,通过较大的润湿引起的坍塌撞击AEV的效果部分地补偿由较小的表面张力诱导的AEV的降低。

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