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1965-1967 年松代地震群中地震电磁现象的因果机制。

Causal mechanisms of seismo-EM phenomena during the 1965-1967 Matsushiro earthquake swarm.

机构信息

Shinshu University, Ueda Campus, 3-15-1 Tokida, Ueda, Nagano, 386-8567, Japan.

Genesis Research Institute, Inc., 4-1-35 Noritake-shinmachi, Nishi-ku, Nagoya, Aichi, 451-0051, Japan.

出版信息

Sci Rep. 2017 Mar 21;7:44774. doi: 10.1038/srep44774.

Abstract

The 1965-1967 Matsushiro earthquake swarm in central Japan exhibited two unique characteristics. The first was a hydro-mechanical crust rupture resulting from degassing, volume expansion of CO/water, and a crack opening within the critically stressed crust under a strike-slip stress. The other was, despite the lower total seismic energy, the occurrence of complexed seismo-electromagnetic (seismo-EM) phenomena of the geomagnetic intensity increase, unusual earthquake lights (EQLs) and atmospheric electric field (AEF) variations. Although the basic rupture process of this swarm of earthquakes is reasonably understood in terms of hydro-mechanical crust rupture, the associated seismo-EM processes remain largely unexplained. Here, we describe a series of seismo-EM mechanisms involved in the hydro-mechanical rupture process, as observed by coupling the electric interaction of rock rupture with CO gas and the dielectric-barrier discharge of the modelled fields in laboratory experiments. We found that CO gases passing through the newly created fracture surface of the rock were electrified to generate pressure-impressed current/electric dipoles, which could induce a magnetic field following Biot-Savart's law, decrease the atmospheric electric field and generate dielectric-barrier discharge lightning affected by the coupling effect between the seismic and meteorological activities.

摘要

日本中部 1965-1967 年的松代地震群表现出两个独特的特征。第一个特征是由于脱气、CO/水的体积膨胀以及在走滑应力下临界应力壳体内的裂缝张开,导致水力学机械壳断裂。另一个特征是,尽管总地震能量较低,但仍发生了复杂的地震电磁(地震 EM)现象,包括地磁强度增加、不寻常的地震光(EQL)和大气电场(AEF)变化。尽管这个地震群的基本破裂过程可以通过水力学机械壳破裂来合理理解,但相关的地震 EM 过程仍在很大程度上未得到解释。在这里,我们描述了一系列涉及水力学机械破裂过程的地震 EM 机制,这些机制是通过将岩石破裂的电相互作用与 CO 气体以及实验室实验中模型化场的介电阻挡放电耦合来观察到的。我们发现,通过岩石新形成的断裂面的 CO 气体会被电化为产生压力感应电流/电偶极子,这可以根据毕奥-萨伐尔定律感应磁场,降低大气电场并产生受地震和气象活动耦合效应影响的介电阻挡放电闪电。

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