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Published July 28, 2006 | Published
Book Section - Chapter Open

Numerical Modeling of Shock-Induced Damage for Granite under Dynamic Loading

Abstract

Johnson-Holmquist constitutive model for brittle materials, coupled with a crack softening model, is used to describe the deviatoric and tensile crack propagation beneath impact crater in granite. Model constants are determined either directly from static uniaxial strain loading experiments, or indirectly from numerical adjustment. Constants are put into AUTODYN-2D from Century Dynamics to simulate the shock-induced damage in granite targets impacted by projectiles at different velocities. The agreement between experimental data and simulated results is encouraging. Instead of traditional grid-based methods, a Smooth Particle Hydrodynamics solver is used to define damaged regions in brittle media.

Additional Information

© 2006 American Institute of Physics. Research supported by NASA/Goddard grant under award no. NNG04GI07G. Contribution No. 9123. Division of Geological and Planetary Sciences, Caltech.

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