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差应力条件下岩石Q值测定方法的改进
引用本文:许昭永,徐东强,包一峰,韩明.差应力条件下岩石Q值测定方法的改进[J].地震研究,1992(4).
作者姓名:许昭永  徐东强  包一峰  韩明
作者单位:云南省地震局 (许昭永,包一峰),唐山工程技术学院采矿系 (徐东强),云南省地震局(韩明)
摘    要:本文指出了脉冲传播和谱振幅比法测定岩石破裂孕育过程中Q值变化矛盾的原因,提出用能量法测定Q值,并以大理岩,大姚铜矿砂岩为例给出了真三轴压缩时岩石破裂孕育过程中P波总能量的变化及不同方法所测Q值的变化特征。其中能量法所测Q值与P波总能量变化特征一致,即主断裂前它们都出现了“下降—回升”变化及变化的各向异性。

关 键 词:Q  值测量谱振幅比法  能量法  P  波总能量

THE IMPROVED DETERMINATION METHOD OF Q-VALUES IN ROCKS UNDER DIFFERENTIAL STRESS
Xu Zhaoyong Sao Yifeng Han Ming.THE IMPROVED DETERMINATION METHOD OF Q-VALUES IN ROCKS UNDER DIFFERENTIAL STRESS[J].Journal of Seismological Research,1992(4).
Authors:Xu Zhaoyong Sao Yifeng Han Ming
Abstract:In this paper, reasons of contradictory Q value variations in the process of rock fracture preparation determined by both the pulse propagation method and spectrum-amplitude ratio method have been pointed out, and the method that uses energy to determine the Q value has been presented. With the granite and sandstone specimens the total P wave energy variation in the process of rock fracture preparation under real triaxial compressions and the characteristic Q value variations by different methods are presented. The Q value by energy method is coincided with the total P wave energy variation, i. e. before the main fracture there all existed a "downfall-rise" variation and variation anisotropy.
Keywords:Q value determination  Spectrum-amplitude ratio method  Energy Method  Total P wave energy
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