多孔介质中地震电变换的实验室研究:1 .过去与未来

IF 1 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
P. A. Kaznacheev, A. N. Kamshilin, A. V. Ponomarev, N. B. Podymova, Z.-Yu. Ya. Maibuk
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引用次数: 0

摘要

摘要:本文介绍了一项致力于多孔介质中地震电变换实验室研究的工作的第一部分。论述了震电变换研究的主要历史阶段和研究现状,以及震电变换在岩石综合力学电磁现象中的地位。提出了一种更新的震电效应分类方法,将震电效应按主要影响场的类型、次要变化的类型以及主要和次要场的频率之比进行划分。提供了每种影响的主要出版物的数据,并指出了当前相关的研究领域。分别介绍了俄罗斯科学院施密特地球物理研究所在机械电磁综合现象中的震电效应研究的历史,以及通讯委员G.A. Sobolev在这些研究中的作用。讨论了与二次电磁场测量有关的主要问题,主要是在实验室实验中。确定了五个最重要的问题,并提出了各种研究人员解决这些问题的方法。研究表明,大多数解决方案是不完整的,进一步的研究应着眼于全面解决这些问题。主要问题是独立测量磁和电分量,以确定地震电效应中二次电磁场的来源。有人建议在实验室中使用一种非接触式测量电流磁效应的方法,并在该领域进行了成功的测试。在该方法中,提出了一些子问题,这些子问题的解对于获得有关震电效应的新数据是必要的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Laboratory Studies of Seismoelectric Transformations in Porous Media: I. Past and Future

Laboratory Studies of Seismoelectric Transformations in Porous Media: I. Past and Future

Abstract—The paper presents the first section of a work devoted to laboratory studies of seismoelectric transformations in porous media. The main historical stages and current state of research into seismoelectric transformations and their place in the aggregate mechanoelectromagnetic phenomena in rocks are considered. An updated classification of seismoelectric effects is proposed, dividing effects by the type of primary influencing field, by the type of secondary changes, and the ratio of the frequencies of the primary and secondary fields. The data on the main publications for each effect are provided, and current relevant research areas are noted. The history of research into seismoelectric effects in the aggregate mechanoelectromagnetic phenomena at the Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, and the role of Corresponding Member G.A. Sobolev in these studies are described separately. The main problems associated with measuring the secondary electromagnetic field, primarily in laboratory experiments, are considered. Five of the most significant problems are identified, and various researchers’ methods for solving them are presented. It is shown that most of the solutions are incomplete and further research should be aimed at a comprehensive solution to these problems. The main problem is independent measurement of the magnetic and electrical components necessary for identifying the sources of the secondary electromagnetic field in the seismoelectric effect. It was proposed to use in the laboratory a contactless measurement of the magnetic effect of electric current, successfully tested earlier in the field. In this proposed method, subproblems have been formulated, the solution of which is necessary to obtain new data on the seismoelectric effect.

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来源期刊
Izvestiya, Physics of the Solid Earth
Izvestiya, Physics of the Solid Earth 地学-地球化学与地球物理
CiteScore
1.60
自引率
30.00%
发文量
60
审稿时长
6-12 weeks
期刊介绍: Izvestiya, Physics of the Solid Earth is an international peer reviewed journal that publishes results of original theoretical and experimental research in relevant areas of the physics of the Earth''s interior and applied geophysics. The journal welcomes manuscripts from all countries in the English or Russian language.
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