汶川8.0级地震前水氡浓度的临界慢化现象研究
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摘要
近年来,临界慢化(Critical slowing down)现象在揭示复杂动力系统是否趋于临界性灾变方面展示了重要潜力.本文基于临界慢化的概念,将其用于水氡浓度观测资料的处理.以2008年5月12日汶川8.0级地震前龙门山断裂带破裂段及附近地区水氡浓度观测点资料为例,分别计算了表征临界慢化现象的自相关系数和方差.结果表明,汶川8.0级地震前,不同台站的水氡浓度震前都存在明显的临界慢化现象,这表明临界慢化现象可能是强地震发生前的一个早期信号.将临界慢化理论引入地震前兆资料的研究,对深入认识地震前兆机理、判定前兆异常所处阶段以及提高地震预测水平都具有重要的现实意义和科学价值.
In recent years,critical slowing down phenomenon have shown great potentials on the aspects of disclosing whether or not a complex dynamic system is tend to critical cataclysm.Based on the concepts of critical slowing down,the observed data of radon concentrations in water were processed in this article.Take radon concentration observation data at Longmen Mountain fault zone and nearby regions before the Wenchuan M_s8.0 earthquake on May 12,2008 as an example, the autocorrelation coefficients and variances which can characterize critical slowing down have been calculated separately.The result indicated that radon data at different station had obviously critical slowing down phenomenon before the Wenchuan M_s8.0 earthquake,which indicated that critical slowing down phenomenon is a possible early warning signal for strong earthquakes.The introduction and study on critical slowing down theory into precursory data processing have practical significances and important scientific values to thoroughly understand precursor mechanism,to determine the stage of precursory anomalies and to enhance earthquake prediction level.
引文
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