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地震前兆时空非均匀性指标Cv值的实验检验
引用本文:王凯英,马胜利,刘力强,马瑾.地震前兆时空非均匀性指标Cv值的实验检验[J].地震学报,2002,24(1):82-89.
作者姓名:王凯英  马胜利  刘力强  马瑾
作者单位:1)中国北京100029中国地震局地质研究所 2)中国北京100029中国地震局构造物理开放实验室
基金项目:地震科学联合基金 ( 95 0 74 35 )资助
摘    要:在双向加载条件下,对两种构造和介质不同的岩石标本进行变形实验,测量了标本表面不同部位的应变.在此基础上,利用王晓青和陈学忠等提出的描述地震前兆非均匀分布的参量————Cv值,分析了标本变形失稳过程中应变异常的分布,以期从实验角度检验Cv值方法并探讨其物理意义.研究表明,Cv值的变化与岩石变形特征的变化有关,是描述前兆分布非均匀性的一种有效指标;Cv值在失稳发生前先异常上升,然后下降,并在Cv值恢复过程中或恢复后伴随着失稳事件的发生.因此,Cv值是一种有效的预报指标. 

关 键 词:岩石力学实验  应变场  地震前兆  非均匀性
文章编号:0253-3782(2002)01-0082-08
修稿时间:2001年1月31日

EXPERIMENTAL EXAMINATION ON THE HETEROG-ENEITY PARAMETER Cv OF DISTRIBUTION OF EARTHQUAKE PRECURSORS
Wang Kaiying , Ma Shengli , Liu Liqiang , Ma Jin , Institute of Geology,China Seismological Bureau,Beijing ,China Laboratory of Tectonophysics,China Seismological Bureau,Beijing ,China.EXPERIMENTAL EXAMINATION ON THE HETEROG-ENEITY PARAMETER Cv OF DISTRIBUTION OF EARTHQUAKE PRECURSORS[J].Acta Seismologica Sinica,2002,24(1):82-89.
Authors:Wang Kaiying  Ma Shengli  Liu Liqiang  Ma Jin  Institute of Geology  China Seismological Bureau  Beijing  China Laboratory of Tectonophysics  China Seismological Bureau  Beijing  China
Institution:Wang Kaiying 1,2) Ma Shengli 1,2) Liu Liqiang 1,2) Ma Jin 1,2) 1) Institute of Geology,China Seismological Bureau,Beijing 100029,China 2) Laboratory of Tectonophysics,China Seismological Bureau,Beijing 100029,China
Abstract:Two rock samples with different structure and materials were deformed under a biaxial loading system, and multipoint strain measurements were performed for each sample. The distribution of strain anomalies during the deformation and the instability process was analyzed by using C v value put forward by Wang Xiaoqing and Chen Xuezhong, et al , a parameter to describe the heterogeneous distribution of earthquake precursors, to examine the method of C v value and to explore its physical meaning experimentally. The result shows that the change of C v value is correlated to the change of deformation characteristics and is an effective parameter to describe the heterogeneity of precursor distribution. C v value increases firstly and then decreases before the instability, and the instability occurs when C v value decreases to the level before increasing. This indicates that C v value may be a useful parameter for earthquake prediction.
Keywords:rock mechanical experiment  strain field  earthquake precursor  heterogeneity
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