Results of 2D Inversion of Data from Deep Electromagnetic Probing with Industrial Power Lines (FENICS Experiment)

IF 0.3 Q4 GEOCHEMISTRY & GEOPHYSICS
A. N. Shevtsov, A. E. Hannibal, T. G. Korotkova, A. A. Skorokhodov
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Abstract

At the stages of the FENICS experiment conducted in 2014 and 2019, unique data on deep electromagnetic sounding with grounded sections of industrial power lines were obtained at distances from 180 to 940 km from the center of the supply line to the measuring installation. The electromagnetic field components were recorded by VMTU-10 measuring equipment (VEGA, St. Petersburg). The fluctuations of the current in the supply line were recorded as a time series with a sampling rate of 1 kHz. Based on synchronous time series of the field components at the observation points and the current strength in the supply vibrator, estimates of the power spectra of the autocorrelation and cross-correlation functions of the recorded values were calculated using fast Fourier transform (FFT). The resulting spectral characteristics were used to determine the amplitudes of the field components of the source and phase shifts between them, as well as to estimate the impedance tensor components. To do this, correction factors were calculated for the ratio of the apparent resistivity values for the horizontal magnetic field component to those for the impedance and electric field. A 2D interpretation is made and estimates of the resistivity allocation at depth are obtained for two sublongitudinal and sublatitudinal profiles of the Karelia–Kola region.

Abstract Image

工业电力线深电磁探测数据二维反演结果(FENICS实验)
在2014年和2019年进行的FENICS实验阶段,从供电线路中心到测量装置的距离为180至940公里,获得了工业电力线路接地部分的深电磁测深独特数据。电磁场分量由VMTU-10测量设备(VEGA,圣彼得堡)记录。供电线路中电流的波动被记录为采样率为1khz的时间序列。基于观测点场分量的同步时间序列和电源振子中的电流强度,利用快速傅里叶变换(FFT)计算记录值的自相关函数和互相关函数的功率谱估计。所得的频谱特性用于确定源的场分量的振幅和它们之间的相移,以及估计阻抗张量分量。为此,计算了水平磁场分量的视电阻率值与阻抗和电场分量的视电阻率值之比的校正因子。对卡累利阿-科拉地区的两个亚纵向和亚纵向剖面进行了二维解释,并获得了深部电阻率分布估计。
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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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