FENICS-2019实验中使用工业架空电力线产生ELF-ULF辐射

IF 0.3 Q4 GEOCHEMISTRY & GEOPHYSICS
V. V. Kolobov, M. B. Barannik, V. V. Ivonin
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引用次数: 0

摘要

在A.A. Zhamaletdinov的指导下,FENICS实验于2007年、2009年、2014年和2019年进行,利用工业架空电力线(OHPL)的接地部分,从供电线路中心到测量装置的距离为180至840公里,获得了独特的深电磁测深数据。在2014年和2019年阶段,使用VMTU-10 (VEGA LLC, St. Petersburg)测量设备记录了源中的电磁场分量和电流强度,该设备允许与GPS参考同步处理测量数据。与之前的阶段不同,在2019年,L-403(摩尔曼斯克-镍)被用作次垂直方向的源,其在许多参数上与之前用于这些目的的L-401不同。本文介绍了利用工业电力线产生用于地球物理研究的极低频-极低频辐射的主要特点。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Generation of ELF–ULF Radiation Using Industrial Overhead Power Lines in the FENICS-2019 Experiment

Generation of ELF–ULF Radiation Using Industrial Overhead Power Lines in the FENICS-2019 Experiment

In the FENICS experiments, performed in 2007, 2009, 2014, and 2019 under the guidance of A.A. Zhamaletdinov, unique deep electromagnetic sounding data were obtained using grounded sections of industrial overhead power lines (OHPL) at distances from 180 to 840 km from the center of the supply line to the measuring installation. At the 2014 and 2019 stages, the components of the electromagnetic field and current strength in the source were recorded with VMTU-10 (VEGA LLC, St. Petersburg) measuring equipment, which allowed synchronous processing of measurement data with GPS referencing. Unlike the previous stages, in 2019, L-403 (Murmansk–Nikel) was used as a source with a sublatitudinal direction, which differs in a number of parameters from L-401, previously used for these purposes. The paper describes the main features of the generation of ELF–ULF radiation for geophysical research using industrial power lines.

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来源期刊
Seismic Instruments
Seismic Instruments GEOCHEMISTRY & GEOPHYSICS-
自引率
44.40%
发文量
45
期刊介绍: Seismic Instruments is a journal devoted to the description of geophysical instruments used in seismic research. In addition to covering the actual instruments for registering seismic waves, substantial room is devoted to solving instrumental-methodological problems of geophysical monitoring, applying various methods that are used to search for earthquake precursors, to studying earthquake nucleation processes and to monitoring natural and technogenous processes. The description of the construction, working elements, and technical characteristics of the instruments, as well as some results of implementation of the instruments and interpretation of the results are given. Attention is paid to seismic monitoring data and earthquake catalog quality Analysis.
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