Numerical modelling of heat generation during shear band formation in rock

Q4 Engineering
T. Saksala, Martina Pressacco, S. Holopainen, R. Kouhia
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引用次数: 2

Abstract

This article gives a computational continuum mechanics answer to a question of how much heat is generated, in terms of temperature rise, during controlled shear band formation in a rock like material. This problem is treated as adiabatic heating due to mechanical dissipation at the material point level. Assuming that only the compressive strength of the rock is temperature dependent, the coupled system of the constitutive equations and the adiabatic heat equation can be solved as a second order polynomial equation for the viscoplastic multiplier at an integration point. A Mohr-Coulomb viscoplastic model with linear softening is employed for rock material description. Numerical simulations of a 2D strip under uniaxial compression at strain rates up to 10 1/s show that the temperature rise in a rock like material with a compressive strength of 100 MPa is less than two degrees.
岩石剪切带形成过程中热量产生的数值模拟
这篇文章给出了一个计算连续体力学的答案,回答了在类岩石材料中受控剪切带形成过程中,根据温度上升,产生了多少热量的问题。由于材料点水平的机械耗散,该问题被视为绝热加热。假设只有岩石的抗压强度与温度有关,本构方程和绝热热方程的耦合系统可以作为粘塑性乘数在积分点的二阶多项式方程求解。采用线性软化的莫尔-库仑粘塑性模型描述岩石材料。对在高达10 1/s的应变速率下单轴压缩的2D条带的数值模拟表明,抗压强度为100MPa的类岩石材料的温升小于2度。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Rakenteiden Mekaniikka
Rakenteiden Mekaniikka Engineering-Mechanical Engineering
CiteScore
0.50
自引率
0.00%
发文量
2
审稿时长
16 weeks
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