Experimental research of natural eigenpolarization electric potential generated during disintegration of frozen sandy-clayey rocks in aqueous media

For studying the mechanism of frozen sandy-clayey rock disintegration, natural electric fields (EP) arising in being frozen wet rocks due to electric potential difference at the boundary between frozen and thawed rocks, were investigated. The performed experiments showed that the frozen sandy-clayey...

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Main Author: V. F. Rochev
Format: Article
Language:English
Published: National University of Science and Technology MISiS 2017-03-01
Series:Горные науки и технологии
Subjects:
Online Access:https://mst.misis.ru/jour/article/view/59
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spelling doaj-7bfb8ca6768c4892b56cd9d35c2ee6592020-11-25T03:28:55ZengNational University of Science and Technology MISiSГорные науки и технологии2500-06322017-03-011515810.17073/2500-0632-2017-1-51-57Experimental research of natural eigenpolarization electric potential generated during disintegration of frozen sandy-clayey rocks in aqueous mediaV. F. Rochev0Technical Institute (branch) of the North-Eastern Federal UniversityFor studying the mechanism of frozen sandy-clayey rock disintegration, natural electric fields (EP) arising in being frozen wet rocks due to electric potential difference at the boundary between frozen and thawed rocks, were investigated. The performed experiments showed that the frozen sandy-clayey rock disintegration in aqueous media is accompanied by generation and changing of natural electric fields in the specimen. In our opinion, the electric field generation is connected with filtration potentials arising as a result of water penetration through pores and fractures into the rock specimen. The eigenpolarization potential measurements were carried out by the potential gradient method using two electrodes frozen into the specimen. As a result, it was proved that the method of measuring the eigenpolarization electric potential difference between two points of a rock specimen has the advantage that it not only indirectly characterizes temperature change in the specimen, but additionally provides information on the process electrokinetics, the dynamics of changes in electrical resistance of the rock between the electrodes, and polarity of different volumes of the rock specimen. In addition, this method allows studying the dynamics of frozen rock thawing, and also confirms the filtration mechanism of frozen rock disintegration in aqueous media.https://mst.misis.ru/jour/article/view/59south yakutiafrozen rocksdisintegrationice contentresearchclay rocksrupturetheory
collection DOAJ
language English
format Article
sources DOAJ
author V. F. Rochev
spellingShingle V. F. Rochev
Experimental research of natural eigenpolarization electric potential generated during disintegration of frozen sandy-clayey rocks in aqueous media
Горные науки и технологии
south yakutia
frozen rocks
disintegration
ice content
research
clay rocks
rupture
theory
author_facet V. F. Rochev
author_sort V. F. Rochev
title Experimental research of natural eigenpolarization electric potential generated during disintegration of frozen sandy-clayey rocks in aqueous media
title_short Experimental research of natural eigenpolarization electric potential generated during disintegration of frozen sandy-clayey rocks in aqueous media
title_full Experimental research of natural eigenpolarization electric potential generated during disintegration of frozen sandy-clayey rocks in aqueous media
title_fullStr Experimental research of natural eigenpolarization electric potential generated during disintegration of frozen sandy-clayey rocks in aqueous media
title_full_unstemmed Experimental research of natural eigenpolarization electric potential generated during disintegration of frozen sandy-clayey rocks in aqueous media
title_sort experimental research of natural eigenpolarization electric potential generated during disintegration of frozen sandy-clayey rocks in aqueous media
publisher National University of Science and Technology MISiS
series Горные науки и технологии
issn 2500-0632
publishDate 2017-03-01
description For studying the mechanism of frozen sandy-clayey rock disintegration, natural electric fields (EP) arising in being frozen wet rocks due to electric potential difference at the boundary between frozen and thawed rocks, were investigated. The performed experiments showed that the frozen sandy-clayey rock disintegration in aqueous media is accompanied by generation and changing of natural electric fields in the specimen. In our opinion, the electric field generation is connected with filtration potentials arising as a result of water penetration through pores and fractures into the rock specimen. The eigenpolarization potential measurements were carried out by the potential gradient method using two electrodes frozen into the specimen. As a result, it was proved that the method of measuring the eigenpolarization electric potential difference between two points of a rock specimen has the advantage that it not only indirectly characterizes temperature change in the specimen, but additionally provides information on the process electrokinetics, the dynamics of changes in electrical resistance of the rock between the electrodes, and polarity of different volumes of the rock specimen. In addition, this method allows studying the dynamics of frozen rock thawing, and also confirms the filtration mechanism of frozen rock disintegration in aqueous media.
topic south yakutia
frozen rocks
disintegration
ice content
research
clay rocks
rupture
theory
url https://mst.misis.ru/jour/article/view/59
work_keys_str_mv AT vfrochev experimentalresearchofnaturaleigenpolarizationelectricpotentialgeneratedduringdisintegrationoffrozensandyclayeyrocksinaqueousmedia
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