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Intermittent dynamics of critical pre-seismic electromagnetic fluctuations

机译:临界地震前电磁波动的间歇动力学

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摘要

It has been proposed that large earthquakes (EQ) are similar to critical phenomena. A new method for the research of the critical fluctuations and for the estimation of corresponding critical exponents is applied to the very high frequency (VHF) electromagnetic (EM) time-series recorder prior to the Kozani-Grevena (K-G) earthquake (EQ) in Greece (M_s = 6.6, on May 13, 1995). Such ruptures involve interactions between structures at many different scales. The system investigated might be considered as possessing two phases. The heterogeneous system first develops isolated cracks, which are nucleated in the weak regions (phase Ⅰ). As the applied strain increases, the cracks join, i.e., long-range correlations are developed between the cracks (phase Ⅱ). A possible phase transition in the fracture process could be elevated by the behavior of the long-range correlations. A basic question in this treatment concerns the critical window in which the transition from the first to the second phase takes place. We argue that the recently proposed intermittent dynamics of critical fluctuations (IDCF)-model indicates the presence of a precursory Critical Window of Stationarity during which the "short-range" correlations evolve to "long-range". The corresponding part of the electromagnetic (EM) time-series reveals: (ⅰ) A remarkable Stationarity, which can be studied in terms of a continuous phase transition at equilibrium. We show that the organization of the precursory EM phenomenon during the phase transition can be described in terms of intermittent dynamics of type Ⅰ. (ⅱ) A power law behavior in the distribution of suitably defined laminar regions and a power spectral density S(f) that can also be approximated by a power-law spectrum S(f) ~ f~(-β). The estimated critical exponents classify the reported critical phase transition to the 3D-Ising-universality class.
机译:已经提出,大地震(EQ)类似于临界现象。研究临界波动和估计相应临界指数的一种新方法被应用于发生在科扎尼-格列韦纳(KG)地震(EQ)之前的甚高频(VHF)电磁(EM)时间序列记录仪。希腊(1995年5月13日,M_s = 6.6)。这种破裂涉及许多不同规模的结构之间的相互作用。被调查的系统可能被认为具有两个阶段。异质系统首先产生孤立的裂纹,并在薄弱区域(Ⅰ相)成核。随着施加的应变的增加,裂纹开始接合,即,裂纹之间形成了长程相关性(Ⅱ相)。远距离相关性的行为可以提高断裂过程中可能的相变。这种处理中的一个基本问题涉及从第一阶段过渡到第二阶段的临界窗口。我们认为,最近提出的间歇波动的临界波动(IDCF)模型表明存在平稳的先验临界窗口,在此期间“短程”相关性演变为“长程”。电磁(EM)时间序列的相应部分显示:(ⅰ)出色的平稳性,可以根据平衡时的连续相变进行研究。我们表明,相变过程中前兆电磁现象的组织可以用Ⅰ型的间歇动力学来描述。 (ⅱ)在适当定义的层流区域的分布中的幂律行为和也可以由幂律谱S(f)〜f〜(-β)近似的幂谱密度S(f)。估计的临界指数将报告的临界相变分类为3D-Ising-大学类。

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