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Binary-medium-based constitutive model of frozen soils subjected to triaxial loading

机译:基于二元介质的冻土三轴荷载本构模型

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To model the elastoplastic behaviors of frozen soils, a binary-medium-based constitutive model is developed and validated by a series of cryotriaxial compressive tests. In the framework of the proposed model, frozen soils are conceptualized to consist of structural blocks and weakened bands. Herein, the structural blocks are idealized as bonded elements with elastic-brittle deformational behaviors. Moreover, the weakened bands are conceptualized as frictional elements whose deformational characteristics are described by a nonlinear Duncan–Chang hyperbolic model. The bonded elements are found to gradually break up and transfer into frictional elements, which collectively contribute to the resistance capability against external loading. From the micro perspective and in the representative volume element (RVE) of the soil specimen, nonuniform strain distributions and particle slippage mechanisms are considered in the strain concentration coefficient and breakage ratio to formulate a constitutive model. Predictions are calibrated with available laboratory results, demonstrating that the proposed model can reasonably account for a breakage mechanism and can quantitatively simulate the nonlinear elastoplastic behavior of frozen soils.
机译:为了模拟冻土的弹塑性行为,建立了基于二元介质的本构模型,并通过一系列低温三轴压缩试验进行了验证。在提出的模型的框架内,冻土被概念化为由结构块和弱化带组成。在此,结构块被理想化为具有弹性-脆性变形行为的结合元件。此外,弱化带被概念化为摩擦元件,其变形特性由非线性邓肯-张双曲模型描述。发现粘结的元件逐渐破裂并转变成摩擦元件,这共同有助于抵抗外部载荷。从微观角度和在土壤标本的代表性体积元(RVE)中,考虑应变集中系数和破损率的不均匀应变分布和颗粒滑移机制,以建立本构模型。根据可用的实验室结果对预测进行校准,这表明所提出的模型可以合理地解释破损机制,并且可以定量地模拟冻土的非线性弹塑性行为。

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