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岩石受力状态对弹性波传播速度的影响初探
引用本文:刘盛东,杨玉岷.岩石受力状态对弹性波传播速度的影响初探[J].煤田地质与勘探,1996,24(5):50-53.
作者姓名:刘盛东  杨玉岷
作者单位:淮南矿业学院,淮南煤电总公司新集煤矿
摘    要:岩石所受的三向应力状态对其弹性波传播性质有一定的影响,此认识为所做的以泥质砂岩、泥岩和硅质胶结的坚硬砂岩为试样的实验所证实。实验结果表明,泥质砂岩和泥岩的vP/vS值几乎保持不变,硬质砂岩的vP/vS曲线却在应力达破坏荷载的90%左右出现下凹现象。经热处理后的硬质砂岩这一下凹现象则更突出

关 键 词:岩石应力状态  弹性波  影响

EXPERIMENT ON INFLUENCE OF STRESS STATES ON ELASTIC WAVE VELOCITY
Liu Shengdong.EXPERIMENT ON INFLUENCE OF STRESS STATES ON ELASTIC WAVE VELOCITY[J].Coal Geology & Exploration,1996,24(5):50-53.
Authors:Liu Shengdong
Institution:Liu Shengdong (Huainan Mining Institute) Yang Yumin Hu Shaolong (Xinji Colliery of the Huainan Coal Electric Corporation)
Abstract:The influenes of triaxial stress states on the elastic wave velocities of clayey sandstone,and claystone and hard siliceous sandstone have been determined by experiments.Claystone and clayey sandstone show hardly any changes in the v P/v sratio.For siliceous sandstone there is a minimum in the ratio of the wave velocities at 90% of the failure stress.This minimum especially present in the siliceous sandstone previously treated with heat.
Keywords:rock  stress state  elastic wave
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