HALL CONDUCTIVITY ESTIMATES FROM MAGNETOTELLURIC SOUNDING DATA

IF 0.8 Q4 GEOCHEMISTRY & GEOPHYSICS Geodynamics & Tectonophysics Pub Date : 2020-12-15 DOI:10.5800/gt-2020-11-4-0509
V. Plotkin, V. Potapov
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引用次数: 1

Abstract

Many minerals have semiconductor properties. It is known that petroleum reservoir rocks permeated with hydrocarbon fluids can sometimes behave as semiconductors. In the Earth’s magnetic field, the electrical conductivity of such materials becomes anisotropic, and the Hall effect is quite possible in rocks in natural conditions and detectable by magnetotelluric sounding. In the anisotropic medium, the field is subject to normal mode splitting, and its components show different attenuation coefficients and phase velocities. The modes differ due to polarization and rotation of the field vectors (clockwise in one mode, and counterclockwise in another). With account of the Hall effect, responses of the medium can be different when the medium is excited by a single normal wave. To detect the Hall effect in MTS surveys, we use the polarization analysis method and select the spectra of modes with right and left circular polarization. Special experiments were carried out to detect the contribution of the Hall effect during the MTS surveys. This article presents the first estimates of the Hall conductivity for the studied rocks.
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根据大地电磁测深资料估计霍尔电导率
许多矿物具有半导体性质。众所周知,油气储层岩石中渗透着烃类流体,有时表现得像半导体。在地球磁场中,这些材料的导电性变得各向异性,霍尔效应在自然条件下的岩石中是很可能存在的,并且可以通过大地电磁测深探测到。在各向异性介质中,场受正模分裂的影响,其分量表现出不同的衰减系数和相速度。由于场矢量的极化和旋转,模式不同(一种模式为顺时针,另一种模式为逆时针)。考虑到霍尔效应,当介质被单一的法向波激发时,介质的响应可能是不同的。为了检测MTS巡天中的霍尔效应,我们采用偏振分析方法,选取了左右圆偏振模式的光谱。在MTS调查期间,进行了专门的实验来检测霍尔效应的贡献。本文给出了所研究岩石霍尔电导率的初步估计。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geodynamics & Tectonophysics
Geodynamics & Tectonophysics GEOCHEMISTRY & GEOPHYSICS-
CiteScore
1.20
自引率
14.30%
发文量
95
审稿时长
24 weeks
期刊介绍: The purpose of the journal is facilitating awareness of the international scientific community of new data on geodynamics of continental lithosphere in a wide range of geolchronological data, as well as tectonophysics as an integral part of geodynamics, in which physico-mathematical and structural-geological concepts are applied to deal with topical problems of the evolution of structures and processes taking place simultaneously in the lithosphere. Complex geological and geophysical studies of the Earth tectonosphere have been significantly enhanced in the current decade across the world. As a result, a large number of publications are developed based on thorough analyses of paleo- and modern geodynamic processes with reference to results of properly substantiated physical experiments, field data and tectonophysical calculations. Comprehensive research of that type, followed by consolidation and generalization of research results and conclusions, conforms to the start-of-the-art of the Earth’s sciences.
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