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原地地应力状态和岩石强度对流体诱发地震活动影响的实验室研究
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作者 K.Masuda O.Nishizawa +2 位作者 k.kusunose T.Satoh 刘希强 《世界地震译丛》 北大核心 1995年第2期24-31,共8页
在水渗入干燥和饱和的花岗岩样品过程中,我们观测到了声发射现象和P波速度变化,以此来研究流体诱发地震活动机制。在流体静压力和高偏应力作用下,分别均匀地将水注入干燥和饱和的圆柱体花岗岩端部表面中,用计算机层析技术揭示的二维P波... 在水渗入干燥和饱和的花岗岩样品过程中,我们观测到了声发射现象和P波速度变化,以此来研究流体诱发地震活动机制。在流体静压力和高偏应力作用下,分别均匀地将水注入干燥和饱和的圆柱体花岗岩端部表面中,用计算机层析技术揭示的二维P波剖面图显示出水前缘皆平行于端部表面,而且在流体静压力作用下,水前缘均匀地离开干燥花岗岩的端部表面。在水注入饱和花岗岩期间,由于受到差应力的作用,岩石内部产生了大量的诱发微裂纹,而对干燥花岗岩却没有产生。声发射源的位置和表面体应变分布显示出诱发微裂纹发生于局部破裂强度较弱的区域。由地下流体流动或水压变化触发的地震活动受控于围岩中既存的原地差应力状态和岩石强度分布。 展开更多
关键词 地震活动性 地应力 岩石强度 对流体
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Effect of Rock Structure on Statistical Characteristics of Acoustic Emission
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作者 k.kusunose O.Nishizawa L.Jouniaux 《Earthquake Research in China》 1999年第3期82-93,共12页
A comparative study on acoustic emission during deformation of two kinds of granites with different structures under triaxial compression was performed using a new acoustic emission recording system with full-waveform... A comparative study on acoustic emission during deformation of two kinds of granites with different structures under triaxial compression was performed using a new acoustic emission recording system with full-waveform record and broad-dynamic range. One is the Inada aplite-granite of homogeneous structure from Japan and the other is the Mayet granite with cemented natural joints from France. For the former granite, acoustic emission events are dispersed randomly and there is no clear clustering along the major fracture. For the latter granite, acoustic emission events are mainly concentrated near the joints. Acoustic emission events occur synchronously with the volumetric dilatation in the former one but far earlier than the volumetric dilatation in the latter one. The two kinds of granites are also clearly different in the frequency spectrum of acoustic emission. The former has a narrower frequency band and a higher frequency component, whereas the latter has a wider frequency band and generally a 展开更多
关键词 ACOUSTIC EMISSION TRIAXIAL compression DILATATION ROCK structure.
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