Dynamic Pulverization of Rock Under Triaxial Static-Stress and High-Rate Shearing

A long-term opening problem in geophysics and engineering is the generation mechanism of rock pulverization (e.g., fault gouge) within the shear zone when subjected to triaxial stress environment and dynamic loads. A novel triaxial Hopkinson bar is developed to apply quasi-static triaxial confinemen...

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Main Authors: Liu, K, Hu, W, Zhao, J
Format: Journal article
Language:English
Published: Springer 2024
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author Liu, K
Hu, W
Zhao, J
author_facet Liu, K
Hu, W
Zhao, J
author_sort Liu, K
collection OXFORD
description A long-term opening problem in geophysics and engineering is the generation mechanism of rock pulverization (e.g., fault gouge) within the shear zone when subjected to triaxial stress environment and dynamic loads. A novel triaxial Hopkinson bar is developed to apply quasi-static triaxial confinement and dynamic loads onto the testing rocks and to measure the energy release from the shearing zone. The results elucidate shear strain-rate threshold (i.e., over 125 s−1) for granite at the triaxial prestress of (10, 10, 10) MPa is required for fine fragments/gouge generation. The effects of shear and normal pre-stresses on dynamic shear strength and surface energy for rock pulverization are investigated, which will help explain fine fragments formed during the high-rate loading events. It is suggested that, except for the quasi-static cumulative slip attrition and multiple dynamic events, rock pulverization or fault gouge could be generated at relatively shallow depths (low geo-stress) in a single dynamic earthquake processes.
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spelling oxford-uuid:923d6eff-554d-4daf-8a80-a7ddd747862e2024-07-11T20:10:43ZDynamic Pulverization of Rock Under Triaxial Static-Stress and High-Rate ShearingJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:923d6eff-554d-4daf-8a80-a7ddd747862eEnglishJisc Publications RouterSpringer2024Liu, KHu, WZhao, JA long-term opening problem in geophysics and engineering is the generation mechanism of rock pulverization (e.g., fault gouge) within the shear zone when subjected to triaxial stress environment and dynamic loads. A novel triaxial Hopkinson bar is developed to apply quasi-static triaxial confinement and dynamic loads onto the testing rocks and to measure the energy release from the shearing zone. The results elucidate shear strain-rate threshold (i.e., over 125 s−1) for granite at the triaxial prestress of (10, 10, 10) MPa is required for fine fragments/gouge generation. The effects of shear and normal pre-stresses on dynamic shear strength and surface energy for rock pulverization are investigated, which will help explain fine fragments formed during the high-rate loading events. It is suggested that, except for the quasi-static cumulative slip attrition and multiple dynamic events, rock pulverization or fault gouge could be generated at relatively shallow depths (low geo-stress) in a single dynamic earthquake processes.
spellingShingle Liu, K
Hu, W
Zhao, J
Dynamic Pulverization of Rock Under Triaxial Static-Stress and High-Rate Shearing
title Dynamic Pulverization of Rock Under Triaxial Static-Stress and High-Rate Shearing
title_full Dynamic Pulverization of Rock Under Triaxial Static-Stress and High-Rate Shearing
title_fullStr Dynamic Pulverization of Rock Under Triaxial Static-Stress and High-Rate Shearing
title_full_unstemmed Dynamic Pulverization of Rock Under Triaxial Static-Stress and High-Rate Shearing
title_short Dynamic Pulverization of Rock Under Triaxial Static-Stress and High-Rate Shearing
title_sort dynamic pulverization of rock under triaxial static stress and high rate shearing
work_keys_str_mv AT liuk dynamicpulverizationofrockundertriaxialstaticstressandhighrateshearing
AT huw dynamicpulverizationofrockundertriaxialstaticstressandhighrateshearing
AT zhaoj dynamicpulverizationofrockundertriaxialstaticstressandhighrateshearing