Laode Ihksan Juarzan
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摘要

[摘要]布莱迪格库乌火山是爪哇的一座泥火山。Bledug Kuwu火山周期性爆发,频率在一分钟内超过5次,指向释放气泡和泥浆。本研究旨在观测Bledug Kuwu火山喷发产生的震电现象的地震和自电位(SP)信号。在Bledug Kuwu泥火山主火山口点附近放置地震传感器进行测量,SP传感器在Bledug Kuwu泥火山主火山口点的垂直,径向和切向放置。分析结果表明,地震事件的主导频率为0.2 Hz,而SP信号的主导频率为48.0 Hz。地震信号和SP信号的到达时间差主要在时间范围内(0,0 ~ 1.5秒),这表明地震信号的出现导致了SP信号的出现,这是震电现象中描述的流体传递的结果。Z分量、NS分量和EW分量的地震事件振幅平均值分别为0.6694、0.4848和0.5158 Count/Volt。Z、NS和EW分量的SP事件振幅平均值分别为1,338、1,249和0,909 mVolt。如果地震事件的振幅大于0.2 Count值,就会出现SP事件。地震事件的幅值与SP事件的幅值成正比,两者的相关系数大于80.0%,地震事件使其路径内的物质产生过大的压力,使物质中的孔隙流体移动,造成电荷分离,是SP信号出现的来源;地震事件的振幅越大,施加在材料上的压力越大,形成的SP事件的振幅也越大,这符合电动力效应机理的震电现象理论。关键词:Bledug Kuwu,自电位(SP),地震,主导频率,不同到达时间,振幅和震电效应。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
ANALISIS SINYAL SEISMIK DAN SELF POTENTIAL (SP) DARI FENOMENA SEIMOELEKTRIK DI GUNUNG LUMPUR BLEDUG KUWU JAWA TENGAH
Abstarct Bledug Kuwu is one of the mud volcano (gunung lumpur) in Java. Bledug Kuwu eruption periodically occured with a frequency of more than five times in one minute, pointed by the release of gas bubbles and mud. This study aims to observe the signals of the seismic and self potential (SP) from seismoelectric phenomenon generated by Bledug Kuwu eruption. Measurements were performed by placed seismic sensor around the main crater point of Bledug Kuwu mud volcano, while the SP sensor placed in the vertical, the radial and tangential direction from the point of the main crater of a Bledug Kuwu mud volcano.. The result of analysis shows that the dominant frequency of seismic events is 0,2 Hz, while dominant frequency of  SP signals is 48,0 Hz. The arrival time difference between seismic and SP signals predominantly in the range of time (0,0 to 1,5 second) which indicates that the appears of the seismic signal causes the appearance of the signal SP as a result of the transfer fluid as described in the seismoelectric phenomenon.The average value of the amplitude of seismic events for Z, NS and EW component is 0,6694, 0,4848 and 0,5158 Count/Volt. The average value of the amplitude of SP events for Z, NS and EW component is 1,338, 1,249 and 0,909 mVolt. SP events will appear if amplitude of seismic events more than 0,2 Count value. Amplitude of sesmic events proportional to the amplitude of the SP event with value of the correlation coefficient between the both is more than 80.0%, the seismic events caused the material in its path have excessive pressure that pore fluid in the material move and cause the separation of charge is the source of the appear of SP signal, the greater the amplitude of the seismic event the pressure exerted on the material so that the larger the amplitude of the SP events formed also getting bigger, this is in accordance with the theory of the seismoelectric phenomenon by electrokinetic effect mechanismKeyword: Bledug Kuwu, Self Potential (SP), seismic, dominant frequency, different arrival time, amplitude and seismoelectric effect.
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