Spatial and temporal characteristics of acoustic emission activity during deforma-tion of rock sampl

来源 :Acta Seismologica Sinica(English Edition) | 被引量 : 0次 | 上传用户:djf344010190
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The spatial and temporal distributions of acoustic emission (AE) during the deformation of samples containing an inhomogeneous fault have been studied under biaxial compression. The results show that the fault strength and the duration from loading to failure increase and the failure mode changes from abrupt instability to gradual failure with increase of lateral stress σ2. The pre-setting fault and its heterogeneity play an important role in controlling AE spatial distribution during the deformation. The basic pattern of AE spatial distribution is controlled by the pre-setting fault, especially the parts with inhomogeneous strength and the strong segment, and the localization of fracturing starts from the positions with inhomogeneous strength. With increase of σ2, the dense AE distribution area spreads from the positions with inhomogeneous strength to the whole strong segment gradually. AE temporal sequence is significantly affected by σ2. The fault shows abrupt instability in final failure, which occurs on a back-ground of ″enhancement-quiescence″ in microfracturing activity at lower σ2. At higher σ2, the fault shows gradual failure, and AE occurrence rate increases continuously and AER increase exponentially before and after the failure. The effect of σ2 on b-value is also remarkable. b-value shows precursory decrease in the weakening stage when fault behavior is abrupt instability, but it shows balanced change when fault behavior is gradual failure. The spatial and temporal distributions of acoustic emission (AE) during the deformation of samples containing an inhomogeneous fault have been investigated under biaxial compression. The results show that the fault strength and the duration from loading to failure increase and the failure mode changes from abrupt instability The pre-setting fault and its heterogeneity play an important role in controlling AE spatial distribution during the deformation. The basic pattern of AE spatial distribution is controlled by the pre-setting fault, especially the parts with inhomogeneous strength and the strong segment, and the localization of fracturing starts from the positions with inhomogeneous strength. With increase of σ2, the dense AE distribution area spreads from the positions with inhomogeneous strength to the whole strong segment gradually. affected by σ2. The fault shows abrupt instability in fina l failure, which occurs on a back-ground of “enhancement-quiescence” in microfracturing activity at lower σ2. At higher σ2, the fault shows gradual failure, and AE occurrence rate increases continuously and AER increase exponentially before and after the failure. effect of σ2 on b-value is also remarkable. b-value shows precursory decrease in the weakening stage when fault behavior is abrupt instability, but it shows balanced change when fault behavior is gradual failure.
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