首页> 外文会议>International Conference on Computational Science - ICCS 2003 Pt.3 Jun 2-4, 2003 Melbourne, Australia and St. Petersburg, Russia >Apparent Strain Localization and Shear Wave Dispersion in Elastic Fault Gouge with Microrotations
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Apparent Strain Localization and Shear Wave Dispersion in Elastic Fault Gouge with Microrotations

机译:微旋转弹性断层泥中的表观应变局部化和剪切波频散

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Shear deformation of fault gouge or other particulate materials often results in observed strain localization, or more precisely, the localization of measured deformation gradients. In conventional elastic materials the strain localization cannot take place therefore this phenomenon is attributed to special types of non-elastic constitutive behaviour. For particulate materials however the Cosserat continuum which takes care of microrotations independent of displacements is a more appropriate model. In elastic Cosserat continuum the localization in displacement gradients is possible under some combinations of the generalized Cosserat elastic moduli. The same combinations of parameters also correspond to a considerable dispersion in shear wave propagation which can be used for independent experimental verification of the proposed mechanism of apparent strain localization in fault gouge.
机译:断层泥或其他颗粒材料的剪切变形通常会导致观察到的应变局部化,或更准确地说,是所测变形梯度的局部化。在常规的弹性材料中,应变局部化无法发生,因此这种现象归因于特殊类型的非弹性本构行为。然而,对于颗粒材料,考虑微旋转而不依赖位移的Cosserat连续体是更合适的模型。在弹性Cosserat连续体中,在广义Cosserat弹性模量的某些组合下,位移梯度的定位是可能的。参数的相同组合还对应于剪切波传播中的相当大的分散,其可用于对断层泥中表观应变局部化所提出的机制进行独立的实验验证。

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