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A thermomechanical anisotropic continuum model for geological materials with multiple joint sets

Journal Article · · International Journal for Numerical and Analytical Methods in Geomechanics
DOI:https://doi.org/10.1002/nag.2795· OSTI ID:1513835
 [1];  [2]
  1. Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
  2. Technion-Israel Institute of Technology, Haifa (Israel)
Joints in geological materials introduce elastic compliance and weak planes on which sliding can occur. Although these materials can have multiple joint sets, they often have preferred orientations that cause both elastic and inelastic anisotropic response even when the unjointed material is isotropic. Azimuthal variations in radial velocity and polarity of tangential motion have been observed in experimental data for wave propagation caused by an initially spherical source in a geological material with multiple joint sets. This observed tangential ground motion was found to be related to mechanical anisotropy caused by preferred orientations of joints in the rock. This paper describes thermomechanical continuum constitutive equations, which model the effects of multiple persistent joint sets. A number of quasi–static examples are considered, which show that the proposed model predicts anisotropic effects of sliding on multiple joint sets similar to those exhibited by computationally expensive mesoscale calculations, which model joint sets explicitly.
Research Organization:
Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)
Sponsoring Organization:
USDOE; USDOE National Nuclear Security Administration (NNSA)
Grant/Contract Number:
AC52-07NA27344
OSTI ID:
1513835
Alternate ID(s):
OSTI ID: 1436814
Report Number(s):
LLNL-JRNL--746369; 930314
Journal Information:
International Journal for Numerical and Analytical Methods in Geomechanics, Journal Name: International Journal for Numerical and Analytical Methods in Geomechanics Journal Issue: 12 Vol. 42; ISSN 0363-9061
Publisher:
WileyCopyright Statement
Country of Publication:
United States
Language:
English

References (14)

Discrete and continuum methods for numerical simulations of non-linear wave propagation in discontinuous media: DISCRETE AND CONTINUUM METHODS journal February 2010
Simple Common Plane contact algorithm: SIMPLE COMMON PLANE CONTACT journal December 2011
A thermomechanical anisotropic model for shock loading of elastic-plastic and elastic-viscoplastic materials with application to jointed rock journal April 2016
An algorithm for continuum modeling of rocks with multiple embedded nonlinearly-compliant joints journal April 2017
Plasticity theory formulated in terms of physically based microstructural variables—Part I. Theory journal October 1994
Modeling added compressibility of porosity and the thermomechanical response of wet porous rock with application to Mt. Helen Tuff journal March 1996
Mechanical and numerical modeling of a porous elastic–viscoplastic material with tensile failure journal March 2000
Practical estimates of rock mass strength journal December 1997
Simulation of penetration into porous geologic media journal April 2007
Generic strength model for dry jointed rock masses journal December 2008
Practical estimates of rock mass strength journal December 1997
Microcrack-induced elastic wave anisotropy of brittle rocks journal March 1995
On the generation of tangential ground motion by underground explosions in jointed rocks journal February 2015
Near-field non-radial motion generation from underground chemical explosions in jointed granite journal September 2017

Figures / Tables (16)


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