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Effects of hysteresis on hydro-mechanical behavior of unsaturated soil

机译:滞后对不饱和土水力 - 力学行为的影响

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Hysteresis is a common feature in the hydraulic properties of unsaturated soils. At a given matric suction, the volumetric water content on a wetting curve is always lower than that on a drying curve. The hysteresis may affect the mechanical behavior and transient process in unsaturated soils. This study focuses on the hysteresis observed in soil-water retention curve (SWRC) tests in the laboratory and inferred from a semi-empirical equation for numerical implementations. Coupled hydro-mechanical finite element analyses, employing an initial drying, main drying, and main wetting curve as hydraulic properties of the soil, were performed to numerically study the effect of hysteresis on the hydro-mechanical behavior of unsaturated soil subjected to water infiltration. Numerical results show that the unsaturated soil exhibits lower soil strength and matric suction distributions when applying the main wetting curve as compared with other SWRCs. The hysteresis appears to affect the stress-strain behavior of the unsaturated soil during prolonged rainfall. Therefore, to predict the instability of the rainfall-induced soil slope more precisely, it is necessary to apply the wetting curve of the SWRC, which shows the hydraulic characteristics of the slope surface.
机译:滞后是不饱和土的液压性能的共同特征。在给定的原料抽吸中,润湿曲线上的体积水含量总是低于干燥曲线上的水含量。滞后可能影响不饱和土壤中的机械特性和瞬态过程。本研究重点介绍在实验室中的土壤 - 水保留曲线(SWRC)测试中观察到的滞后,并从半经验方程推断出用于数值实现的。耦合的水力机械有限元分析,采用初始干燥,主干和主要润湿曲线作为土壤的液压性能进行,以数值研究滞后对不饱和土水渗透的液压力学的影响。数值结果表明,与其他SMRC相比,不饱和土在施加主要润湿曲线时表现出降低的土壤强度和原木吸附分布。滞后似乎影响了不饱和土的长度降雨期间的应力 - 应变行为。因此,为了更精确地预测降雨诱导的土坡的不稳定性,需要施加SWRC的润湿曲线,其表示斜面表面的液压特性。

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