{"title":"Thermo-poro-mechanical analysis of rapid fault deformation","authors":"I. Vardoulakis","doi":"10.1201/9781003077497-68","DOIUrl":null,"url":null,"abstract":"In this paper the basic mathematical structure of a thermo-poro-mechanical model for faults under rapid shear is discussed. The analysis is 1D in space and concerns the infinitely extended fault. The gauge material is considered as a two-phase material consisting of a thermo-elastic fluid and of a thermoporo-elasto-viscoplastic skeleton. The governing equations are derived from first principles, expressing mass, energy and momentum balance inside the fault. They are a set of coupled diffusion-generation equations that contain three unknown functions, the pore-pressure, the temperature and the velocity field inside the fault. The original mathemetically ill-posed problem is regularized using a viscous-type and a 2 gradient regularization. Numerical results are presented and discussed. ) t , z ( p , the temperature ) t , z ( θ and the velocity ) t , z ( v are assumed to be functions only of the time t and of the position z in normal to the band direction (Figure 1). Figure 1. The deforming shear-band with heat and fluid fluxes As is shown in Vardoulakis (2000) mass and energy balance equations together with Darcy's and Fourier's laws lead to a set of coupled diffusiongeneration equations for the pore-water pressure ) t , z ( p and the temperature field ) t , z ( θ inside the shear band. For easy reference we summarize here these equations and define the pertinent material parameters.","PeriodicalId":166080,"journal":{"name":"Powders and Grains 2001","volume":"2 5","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2020-09-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Powders and Grains 2001","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1201/9781003077497-68","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1
Abstract
In this paper the basic mathematical structure of a thermo-poro-mechanical model for faults under rapid shear is discussed. The analysis is 1D in space and concerns the infinitely extended fault. The gauge material is considered as a two-phase material consisting of a thermo-elastic fluid and of a thermoporo-elasto-viscoplastic skeleton. The governing equations are derived from first principles, expressing mass, energy and momentum balance inside the fault. They are a set of coupled diffusion-generation equations that contain three unknown functions, the pore-pressure, the temperature and the velocity field inside the fault. The original mathemetically ill-posed problem is regularized using a viscous-type and a 2 gradient regularization. Numerical results are presented and discussed. ) t , z ( p , the temperature ) t , z ( θ and the velocity ) t , z ( v are assumed to be functions only of the time t and of the position z in normal to the band direction (Figure 1). Figure 1. The deforming shear-band with heat and fluid fluxes As is shown in Vardoulakis (2000) mass and energy balance equations together with Darcy's and Fourier's laws lead to a set of coupled diffusiongeneration equations for the pore-water pressure ) t , z ( p and the temperature field ) t , z ( θ inside the shear band. For easy reference we summarize here these equations and define the pertinent material parameters.
本文讨论了快速剪切作用下断层热孔力学模型的基本数学结构。该分析在空间上是一维的,涉及到无限扩展的断层。压力表材料被认为是由热弹性流体和热弹性-弹-粘塑性骨架组成的两相材料。控制方程由第一性原理导出,表达了断层内部的质量、能量和动量平衡。它们是一组耦合的扩散生成方程,包含断层内部的孔隙压力、温度和速度场三个未知函数。利用粘滞型正则化和2梯度正则化对原数学病态问题进行正则化。给出了数值结果并进行了讨论。假设t, z (p,温度)t, z (θ)和速度)t, z (v)仅是时间t和位置z垂直于带方向的函数(图1)。根据Vardoulakis(2000)的质量和能量平衡方程,结合Darcy定律和Fourier定律,可以得到剪切带内孔隙水压力t, z (p)和温度场t, z (θ)的耦合扩散生成方程。为了方便参考,我们在这里总结了这些方程并定义了相关的材料参数。