意大利南部震区电学和地震学参数遥感测控站的新原型设计

M. Balasco , D. Chianese , V. Cuomo , G. Di Bello , M.R. Gallipoli , V. Lapenna , M. Mucciarelli
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引用次数: 5

摘要

在本文中,我们描述了一种能够联合探测电震参数的新型遥感站的主要特征。该测量站已安装在亚平宁南部链的铁托站点,这是地中海地区地震最活跃的地区之一;它结合了新的数据采集技术和鲁棒的统计技术来区分记录信号中的异常波动和背景噪声。全自动台站配备了能够检测自电位信号的传感器(16通道,A/D 24位,采样率0.25Hz)和连接到具有133 dB动态的采集单元的1Hz三方向地震仪。经过初步的过滤程序,主要是为了消除由于气象气候参数和/或文化电噪声造成的所有影响,一个专门开发的软件用于研究电信号异常模式与当地微地震活动之间可能的相关性。特别是,新台站的仪器特征使我们能够将在短时间尺度上检测到的电信号波动与国家地震网(国家地球物理研究所)没有揭示的低震级地震事件(M<3)进行比较。对1999年首次观测结果的分析表明,该台站在地震活动性地区的地球物理监测网中具有较大的应用价值。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Design of a new prototype of remote station to detect electrical and seismometric parameters in a seismic area of Southern Italy

In this work we describe the main features of a new prototype of remote station able to jointly detect electrical and seismometric parameters. The measuring station has been installed at Tito site on the Southern Apennine chain, one of the most seismic active areas of the Mediterranean region; it combines new technologies for the data acquisition with a robust statistical technique to discriminate anomalous fluctuations from background noise in the recorded signals. The completely automatic station is equipped with sensors able to detect self-potential signals (16 channels, A/D 24 bit, sampling rate of 0.25Hz) and a 1Hz three directional seismometer connected to an acquisition unit having a dynamics of 133 dB. After a preliminary filtering procedure, mainly devoted to remove all the influences due to meteo-climatic parameters and/or cultural electrical noise, a software developed ad hoc to study the possible correlation between anomalous patterns in electrical signals and local microseismic activity was employed. In particular, the instrumental features of the new station allow us to compare the fluctuations of electrical signal, detected at short temporal scales, with seismic events with low magnitude (M<3), that are not revealed by the national seismometric network (National Institute of Geophysics). The analysis of the first results obtained during the 1999 confirms us that the station could be largely used in a geophysical monitoring network operating in seismic active areas.

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