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Evaluation of capillary water retention effects on the development of the suction stress characteristic curve

机译:评价毛细管水保留对吸力特性曲线发展的影响

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摘要

The suction stress characteristic framework is a practical approach for relating the suction and the water-filled pore volume to the stress state of unsaturated soils. It predicts the effective stress by developing the suction stress characteristic curve from the soil-water retention curve. In this framework, the effective degree of saturation is usually calculated by the empirical water retention model of van Genuchten (published in 1980). In this paper, the use of a generalized soil-water retention model proposed by Lu in 2016, which differentiates the role of capillary and adsorption mechanisms, in the suction stress characteristic framework is studied. A redefinition of the effective degree of saturation is suggested, by choosing the retention state where capillarity approaches zero instead of the residual retention state. The validity of this assumption is examined using experimental data obtained by unsaturated shear strength and retention tests and datasets collected from the literature. The proposed definition is applicable for a variety of soils where capillarity is the dominant mechanism in producing suction stress within the range of suction 0-1500 kPa. In addition, it is observed that the generalized soil-water retention model presents a more realistic prediction of unsaturated shear strength compared with empirical water retention models.
机译:吸力-应力特征框架是将吸力和充水孔隙体积与非饱和土的应力状态联系起来的一种实用方法。通过从土壤水分保持曲线发展吸力-应力特征曲线,预测有效应力。在此框架下,有效饱和度通常由van Genuchten(1980年出版)的经验持水模型计算。本文研究了在吸力-应力特征框架中使用Lu在2016年提出的广义土壤水分保持模型,该模型区分了毛细和吸附机制的作用。建议重新定义有效饱和度,选择毛细接近零的保留状态,而不是残余保留状态。通过非饱和抗剪强度和保持力试验获得的实验数据以及从文献中收集的数据集,验证了该假设的有效性。建议的定义适用于各种土壤,其中毛细作用是在吸力0-1500 kPa范围内产生吸力应力的主要机制。此外,与经验持水模型相比,广义土壤持水模型对非饱和剪切强度的预测更为真实。

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