首页> 外文会议>International Conference on Atmospheric Electricity >ON ATMOSPHERIC ELECTRIC FIELD ANOMALY BEFORE THE CARPATHIAN EARTHQUAKE OF 30. 08. 1986 AT THE POLISH OBSERVATORY (S)WIDER
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ON ATMOSPHERIC ELECTRIC FIELD ANOMALY BEFORE THE CARPATHIAN EARTHQUAKE OF 30. 08. 1986 AT THE POLISH OBSERVATORY (S)WIDER

机译:1986年喀尔巴阡地震前的大气电场异常的研究

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Atmospheric electric field (Ez ) anomalies before earthquakes are classified as immediate precursors of earthquakes. However, there are not enough data on these anomalies due to significant influence of factors of meteorological and magnetospheric origin which might obscure or mask relations anomalies to seismic activity. Therefore, it still remains an urgent task to accumulate evidence on Ez anomalies in different geological and geophysical conditions and to refine models of electromagnetic earthquake precursors. The retrospective analysis of Ez data was conducted for 3 last great Carpathian earthquakes (4. 03. 1977, 30. 08.1986, 30. 05. 1990) with this aim at the Polish observatory (S)wider. Only the event on 30. 08. 1986 satisfied fair-weather and quiet geomagnetic conditions. Noticeable Ez anomaly (from –250 V/m to +750 V/m) was observed from 02 to 16 UT before this earthquake (origin time 21. 28 UT). The mechanism of such anomalies is still mysterious. However, authors point to massive emissions of ions from crystalline structures under variable stress and temperature, and to electric polarization and current phenomena in the rocks/ground, which may transfer charge anomalies to the surface and then, via atmosphere, change the electric field over the ground at considerable areas.
机译:地震之前的大气电场(Ez)异常被分类为地震的直接先兆。但是,由于气象和磁层起源因素的重大影响,这些异常可能没有足够的数据,这些因素可能掩盖或掩盖了与地震活动的关系异常。因此,在不同的地质和地球物理条件下积累有关Ez异常的证据并完善电磁地震前兆的模型仍然是紧迫的任务。对最近3次喀尔巴阡大地震(4. 03. 1977,30. 08.1986,30. 05. 1990)的Ez数据进行了回顾性分析,目的是在更广阔的波兰天文台进行观测。仅在1986年8月30日的事件满足了晴天和安静的地磁条件。在地震发生之前的02至16 UT(起源时间21. 28 UT)观察到明显的Ez异常(从–250 V / m到+750 V / m)。这种异常的机制仍然是未知的。然而,作者指出,在可变的应力和温度下,晶体结构会大量释放离子,岩石/地面中的电极化和电流现象可能会将电荷异常转移到表面,然后通过大气层改变电场。在相当大的区域地面。

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