skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Equivalent Continuum Modeling for Shock Wave Propagation in Jointed Media

Technical Report ·
DOI:https://doi.org/10.2172/969829· OSTI ID:969829

This study presents discrete and continuum simulations of shock wave propagating through jointed media. The simulations were performed using the Lagrangian hydrocode GEODYN-L with joints treated explicitly using an advanced contact algorithm. They studied both isotropic and anisotropic joint representations. For an isotropically jointed geologic medium, the results show that the properties of the joints can be combined with the properties of the intact rock to develop an equivalent continuum model suitable for analyzing wave propagation through the jointed medium. For an anisotropically jointed geologic medium, they found it difficult to develop an equivalent continuum (EC) model that matches the response derived from mesoscopic simulation. They also performed simulations of wave propagation through jointed media. Two appraoches are suggested for modeling the rock mass. In one approach, jointed are modeled explicitly in a Lagrangian framework with appropriate contact algorithms used to track motion along the interfaces. In the other approach, the effect of joints is taken into account using a constitutive model derived from mesoscopic simulations.

Research Organization:
Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
Sponsoring Organization:
USDOE
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
969829
Report Number(s):
LLNL-TR-421505; TRN: US201002%%1016
Country of Publication:
United States
Language:
English

Similar Records

NEAR FIELD MODELING OF SPE1 EXPERIMENT AND PREDICTION OF THE SECOND SOURCE PHYSICS EXPERIMENTS (SPE2)
Technical Report · Thu Oct 20 00:00:00 EDT 2011 · OSTI ID:969829

Comparison of Joint Modeling Approaches Including Eulerian Sliding Interfaces
Technical Report · Wed Dec 16 00:00:00 EST 2009 · OSTI ID:969829

A thermomechanical anisotropic continuum model for geological materials with multiple joint sets
Journal Article · Thu May 10 00:00:00 EDT 2018 · International Journal for Numerical and Analytical Methods in Geomechanics · OSTI ID:969829