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Model for Lateral Swelling Pressure in Unsaturated Expansive Soils

机译:不饱和膨胀土横向膨胀压力模型

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Unsaturated expansive soils annually cause major economic losses and structural damages to foundations and earthen structures, primarily due to exhibiting large amounts of swelling and shrinkage when subjected to variations in water content. If an expansive soil is laterally constrained, lateral swelling pressure can exacerbate the unfavorable characteristics of expansive soil by increasing the lateral earth pressure applied to geotechnical structures. This study presents a model to determine lateral swelling pressure considering transient flow in deformable (swelling) unsaturated soils. The transient profiles of water content and suction versus depth during the wetting process are determined considering a coupled hydromechanical behavior. The interplay between the soil deformation, water content, and hydraulic conductivity is accounted for by linking the soil swelling-shrinkage characteristic curve (SSSCC), the soil water retention curve (SWRC), and the hydraulic conductivity function (HCF). An analytical model for quantifying lateral swelling pressure is then developed using a suction stress-based effective stress, the SWRC, and extended Hook's law for unsaturated soils. The presented model is built upon the conceptual model that lateral swelling pressure is controlled by infiltration-induced changes in suction stress of a laterally-constrained unsaturated soil. The model offers a generalized framework to determine lateral swelling pressure of expansive soils under different degrees of saturation while accounting for the effect of deformation on water content and suction profiles. The model is validated against results attained from three sets of experimental tests available in the literature. Through the three case studies examined, the proposed model exhibited a reasonable accuracy over a wide range of degrees of saturation from 50% to near fully saturated conditions. The findings of this study can contribute toward more accurate evaluations regarding the performance of geotechnical structures in unsaturated expansive soils.
机译:不饱和膨胀的土壤每年对基础和土壤结构的主要经济损失和结构性损害,主要是由于当经受水含量的变化时表现出大量的溶胀和收缩。如果膨胀的土壤横向约束,则横向溶胀压力可以通过增加施加到岩土结构的横向接地压力来加剧膨胀土的不利特征。本研究提出了一种模型,以确定考虑变形(膨胀)不饱和土壤中的瞬态流动的横向膨胀压力。考虑到耦合的流体机械行为,确定润湿过程中的含水量和吸入与深度的瞬态谱。通过将土壤溶胀收缩特性曲线(SSSCC),土壤水保留曲线(SWRC)和液压导电功能(HCF)连接,占土壤变形,含水量和液压导率之间的相互作用。然后使用基于抽吸应力的有效应力,SWRC和延长的钩子定律来开发用于量化横向溶胀压力的分析模型。所提出的模型基于概念模型,即通过渗透引起的横向约束的不饱和土的吸入应力的变化来控制横向溶胀压力。该模型提供了广义框架,用于在不同饱和度下确定膨胀土的横向膨胀压力,同时占变形对水含量和吸力剖面的影响。该模型验证了从文献中提供的三组实验测试所获得的结果。通过检查三种案例研究,所提出的模型在各种饱和度范围内的可合理精度从50%到近乎完全饱和的条件。该研究的结果可以有助于对不饱和膨胀土壤岩土结构性能的更准确的评估。

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