Group B, Poster #134, Fault and Rupture Mechanics (FARM)
Multiscale Dynamics of 3D Rupture Zones using a Continuum Damage Breakage Rheology
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Poster Presentation
2024 SCEC Annual Meeting, Poster #134, SCEC Contribution #13808 VIEW PDF
tions using damage (cracking) and breakage (granulation) variables, partitioning strain energy into damaged (visco-)elastic and granular phases. We focus on how depth-dependent variations in normal stress, temperature, and pore pressure influence damage evolution, energy dissipation, and ground motion, aiming to connect surface observations and seismicity to subsurface physics.
The 3D CDBM is implemented in our dynamic rupture simulator DynamicCDBM and DynamicCDBM_F. In DynamicCDBM, pre-existing fault zones are modeled as damaged tubular regions, and dynamic ruptures are nucleated by slightly increasing the damage in a localized region; slip and slip rates are computed from the strain across damage bands as solid-granular phase transitions occur. In DynamicCDBM_F, pre-existing faults are represented as discontinuous cohesive zone interfaces whose behavior is governed by friction laws. The off-fault simulation domains in both cases are governed by CDBM, allowing damage to heal or grow, in arbitrary directions, independent of the underlying mesh, with evolving deformation. While the damage zone thickness remains relatively narrow, it has a significant impact on rupture physics including enhancement of high-frequency waves, generation of isotropic source components, and manipulation of rupture speed and mode. The simulators developed in this study are available on the Quakeworx science gateway for democratizing access to earthquake simulations and data.
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The 3D CDBM is implemented in our dynamic rupture simulator DynamicCDBM and DynamicCDBM_F. In DynamicCDBM, pre-existing fault zones are modeled as damaged tubular regions, and dynamic ruptures are nucleated by slightly increasing the damage in a localized region; slip and slip rates are computed from the strain across damage bands as solid-granular phase transitions occur. In DynamicCDBM_F, pre-existing faults are represented as discontinuous cohesive zone interfaces whose behavior is governed by friction laws. The off-fault simulation domains in both cases are governed by CDBM, allowing damage to heal or grow, in arbitrary directions, independent of the underlying mesh, with evolving deformation. While the damage zone thickness remains relatively narrow, it has a significant impact on rupture physics including enhancement of high-frequency waves, generation of isotropic source components, and manipulation of rupture speed and mode. The simulators developed in this study are available on the Quakeworx science gateway for democratizing access to earthquake simulations and data.
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