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岩石受力状态对弹性波传播速度影响的初步研究
引用本文:刘盛东,杨玉岷.岩石受力状态对弹性波传播速度影响的初步研究[J].中国煤田地质,1996,8(3):48-51.
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。为保证岩石中存在微隙,对部分试样还作了高温预热处理。实验结果表明,泥质砂岩和泥岩的V_p/V_s值几乎保持不变,但坚硬砂岩的V_p/V_s值曲线却在应力达破坏荷载的90%左右时出现下凹现象,经热处理的硬砂岩的这一下凹现象则更突出。

关 键 词:弹性波速,岩石,应力状态,V_p/V_s比值

Experiment on Influence of Stress States on Elastic Waves Velocity
Liu Shengdong.Experiment on Influence of Stress States on Elastic Waves Velocity[J].Coal Geology of China,1996,8(3):48-51.
Authors:Liu Shengdong
Abstract:The influence of triaxiale stress states on the elastic waves velocities of clayey sandstone,claystone and hard siliceous sandstone has been determined by experiments.Some samples are previ-ously treated with heat to intendify crack prodution.Claystone and clayey sandstone show hardly anychanges in the V_p/V_s ratio.For siliceous sandstone there is a minimum in the ratio of the wave veloci-ties at sbout 90%of the failure stress.This minimum especially present in thesiliceous santone previ-ously treated with heat.
Keywords:the elastic wave velocity stress state V_p/V_s ratio  
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