Active ultrasonic monitoring in rock joints and gouge materials has the potential to detect the signatures of shear failure for a wide range of sliding modes,from slow and stable movements to fast and unstable sliding...Active ultrasonic monitoring in rock joints and gouge materials has the potential to detect the signatures of shear failure for a wide range of sliding modes,from slow and stable movements to fast and unstable sliding.While these collected measurements currently are being used to identify the seismic precursors to shear failure in rock joints and gouge materials,the underlying physical processes and contact scale mechanisms that control the changes in ultrasonic wave attributes are still poorly understood.To address this knowledge gap,this paper aims to investigate the relationship between the variations in ultrasonic wave attributes and the underlying particle scale mechanisms during both compression and shearing.Our double direct shear experiments were coupled with ultrasonic wave propagation measurements on granular quartz gouges,in which the gouge layers were sheared under different sliding velocities and constant normal stress conditions.Simultaneously,ultrasonic waveforms were continuously recorded during shearing with a fast data acquisition system and three pairs of ultrasonic wave transducers embedded at the two sides of the gouge layers.Different particle comminution mechanisms were observed from the non-uniform distribution of normal and shear stresses through the changes in ultrasonic transmissivity and scanning electron microscope(SEM)images.Our results show that the signatures of the geometry-and time-dependent variations of the inter-particle contact quality and pore volume changes with sliding velocity and slip accumulation were clearly captured from the variations in the transmitted wave amplitude and the dominant frequency,respectively.In addition,we found that variations in dominant frequency corresponded to dilation and compaction of the granular gouge layer during compression as well as stable and unstable sliding.Our results therefore confirmed that nondestructive acoustic techniques are capable of capturing a variety of micromechanical processes during fault gouge deformation and may prove useful in natural settings.展开更多
基金The authors would like to acknowledge the supports provided by the Southern California Earthquake Center(Grant No.17242)the U.S.Department of Energy(Grant No.DE-SC0019117).
文摘Active ultrasonic monitoring in rock joints and gouge materials has the potential to detect the signatures of shear failure for a wide range of sliding modes,from slow and stable movements to fast and unstable sliding.While these collected measurements currently are being used to identify the seismic precursors to shear failure in rock joints and gouge materials,the underlying physical processes and contact scale mechanisms that control the changes in ultrasonic wave attributes are still poorly understood.To address this knowledge gap,this paper aims to investigate the relationship between the variations in ultrasonic wave attributes and the underlying particle scale mechanisms during both compression and shearing.Our double direct shear experiments were coupled with ultrasonic wave propagation measurements on granular quartz gouges,in which the gouge layers were sheared under different sliding velocities and constant normal stress conditions.Simultaneously,ultrasonic waveforms were continuously recorded during shearing with a fast data acquisition system and three pairs of ultrasonic wave transducers embedded at the two sides of the gouge layers.Different particle comminution mechanisms were observed from the non-uniform distribution of normal and shear stresses through the changes in ultrasonic transmissivity and scanning electron microscope(SEM)images.Our results show that the signatures of the geometry-and time-dependent variations of the inter-particle contact quality and pore volume changes with sliding velocity and slip accumulation were clearly captured from the variations in the transmitted wave amplitude and the dominant frequency,respectively.In addition,we found that variations in dominant frequency corresponded to dilation and compaction of the granular gouge layer during compression as well as stable and unstable sliding.Our results therefore confirmed that nondestructive acoustic techniques are capable of capturing a variety of micromechanical processes during fault gouge deformation and may prove useful in natural settings.
