Comminution‐Induced Transient Frictional Behavior in Sheared Granular Halite

Abstract Grain comminution is commonly observed in numerous geological settings. To elucidate the role of grain comminution in dry granular friction, we sheared breakable halite (NaCl) grains using a ring‐shear configuration at a constant slip rate under various normal stresses. We observed transien...

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Main Authors: Chengrui Chang, Hiroyuki Noda, Yohei Hamada, Chao Huang, Tao Ma, Gonghui Wang, Tetsuo Yamaguchi
Format: Article
Language:English
Published: Wiley 2024-11-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2024GL109645
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author Chengrui Chang
Hiroyuki Noda
Yohei Hamada
Chao Huang
Tao Ma
Gonghui Wang
Tetsuo Yamaguchi
author_facet Chengrui Chang
Hiroyuki Noda
Yohei Hamada
Chao Huang
Tao Ma
Gonghui Wang
Tetsuo Yamaguchi
author_sort Chengrui Chang
collection DOAJ
description Abstract Grain comminution is commonly observed in numerous geological settings. To elucidate the role of grain comminution in dry granular friction, we sheared breakable halite (NaCl) grains using a ring‐shear configuration at a constant slip rate under various normal stresses. We observed transient frictional behaviors: a constant regime exhibiting a high friction coefficient at small slip displacements, and a weakening regime showing a substantial decay in friction at large slip displacements. The characteristic slip lengths for both regimes decreased with normal stress and were characterized by similar exponents. Micro‐X‐ray tomography revealed the evolution of microstructure from distributed grain comminution to progressive shear localization for these two regimes. We propose that the filling processes of comminuted fine particles, during which fine particles saturate and then overflow the shear zone, define transient frictional behaviors. This study may hold significant implications for natural shear systems, given the ubiquity of comminution and localization phenomena.
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language English
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series Geophysical Research Letters
spelling doaj-art-996372322d8345a1ac9cda3d6c21b3102025-08-20T03:16:26ZengWileyGeophysical Research Letters0094-82761944-80072024-11-015121n/an/a10.1029/2024GL109645Comminution‐Induced Transient Frictional Behavior in Sheared Granular HaliteChengrui Chang0Hiroyuki Noda1Yohei Hamada2Chao Huang3Tao Ma4Gonghui Wang5Tetsuo Yamaguchi6Department of Biomaterial Sciences Graduate School of Agricultural and Life Sciences The University of Tokyo Tokyo JapanDisaster Prevention Research Institute Kyoto University Uji JapanKochi Institute for Core Sample Research Japan Agency for Marine‐Earth Science and Technology (JAMSTEC) Nankoku JapanDivision of Earth and Planetary Sciences Graduate School of Science Kyoto University Uji JapanInstitute of Modern Physics Chinese Academy of Sciences Lanzhou ChinaDisaster Prevention Research Institute Kyoto University Uji JapanDepartment of Biomaterial Sciences Graduate School of Agricultural and Life Sciences The University of Tokyo Tokyo JapanAbstract Grain comminution is commonly observed in numerous geological settings. To elucidate the role of grain comminution in dry granular friction, we sheared breakable halite (NaCl) grains using a ring‐shear configuration at a constant slip rate under various normal stresses. We observed transient frictional behaviors: a constant regime exhibiting a high friction coefficient at small slip displacements, and a weakening regime showing a substantial decay in friction at large slip displacements. The characteristic slip lengths for both regimes decreased with normal stress and were characterized by similar exponents. Micro‐X‐ray tomography revealed the evolution of microstructure from distributed grain comminution to progressive shear localization for these two regimes. We propose that the filling processes of comminuted fine particles, during which fine particles saturate and then overflow the shear zone, define transient frictional behaviors. This study may hold significant implications for natural shear systems, given the ubiquity of comminution and localization phenomena.https://doi.org/10.1029/2024GL109645granular frictioncomminutionshear localizationhaliteslip weakening
spellingShingle Chengrui Chang
Hiroyuki Noda
Yohei Hamada
Chao Huang
Tao Ma
Gonghui Wang
Tetsuo Yamaguchi
Comminution‐Induced Transient Frictional Behavior in Sheared Granular Halite
Geophysical Research Letters
granular friction
comminution
shear localization
halite
slip weakening
title Comminution‐Induced Transient Frictional Behavior in Sheared Granular Halite
title_full Comminution‐Induced Transient Frictional Behavior in Sheared Granular Halite
title_fullStr Comminution‐Induced Transient Frictional Behavior in Sheared Granular Halite
title_full_unstemmed Comminution‐Induced Transient Frictional Behavior in Sheared Granular Halite
title_short Comminution‐Induced Transient Frictional Behavior in Sheared Granular Halite
title_sort comminution induced transient frictional behavior in sheared granular halite
topic granular friction
comminution
shear localization
halite
slip weakening
url https://doi.org/10.1029/2024GL109645
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