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Three-dimensional noncoaxial plasticity modeling of shear band formation in geomaterials

机译:岩土材料中剪切带形成的三维非同轴塑性建模

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摘要

Accurate prediction of shear band formation in geomaterials is crucial in the solution of various stability problems in geotechnical engineering. The initiation of shear band is strongly dependent on the constitutive description of the prelocalization homogeneous deformation. Conventional plasticity models assume that coaxiality exists between the directions of principal stresses and the directions of plastic strain increments. Accumulating evidence has however shown that this assumption is not appropriate. In this paper, a noncoaxial constitutive modeling platform is presented in a general three-dimensional stress space. It is shown that the classical vertex-like structure, which has been widely adopted to describe the noncoaxial constitutive response, only represents the two-dimensional condition. Examples are presented to demonstrate the capability of the modeling platform in capturing the initiation and orientation of shear band in a granular soil. The significance of the noncoaxiality effects is illustrated by comparisons of the predictions produced by coaxial and noncoaxial (both two-dimensional and three-dimensional) plasticity models.
机译:在解决岩土工程中各种稳定性问题时,准确预测土工材料中的剪切带形成至关重要。剪切带的产生强烈取决于预定位均质变形的本构描述。传统的可塑性模型假定主应力方向与塑性应变增量方向之间存在同轴性。但是,越来越多的证据表明这种假设是不合适的。在本文中,提出了在一般三维应力空间中的非同轴本构建模平台。结果表明,被广泛用于描述非同轴本构响应的经典顶点状结构仅代表二维条件。给出了一些实例来说明建模平台捕获粒状土壤中剪切带的起始和定向的能力。通过比较同轴和非同轴(二维和三维)塑性模型所产生的预测,可以说明非同轴效应的重要性。

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