Relaxation phenomena of electrical signal emissions from rock following application of abrupt mechanical stress

<p>The emission of electrical signals during application of mechanical stress to brittle geo-materials (the so-called pressure-stimulated current; PSC) can provide significant information regarding the mechanical status of a studied rock sample. PSCs originate as a result of the openin...

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Main Authors: George Hloupis, Ilias Stavrakas, Filippos Vallianatos, Dimos Triantis
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 2012-04-01
Series:Annals of Geophysics
Subjects:
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/5316
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spelling doaj-0bce633c202c42eda922306e6646e0832020-11-24T23:36:38ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X2012-04-0155110.4401/ag-5316Relaxation phenomena of electrical signal emissions from rock following application of abrupt mechanical stressGeorge HloupisIlias StavrakasFilippos VallianatosDimos Triantis<p>The emission of electrical signals during application of mechanical stress to brittle geo-materials (the so-called pressure-stimulated current; PSC) can provide significant information regarding the mechanical status of a studied rock sample. PSCs originate as a result of the opening of cracks and microfractures in rock. In this study, such electrical signal emissions are detected and studied when rock samples are subjected to step-wise mechanical stress, increased from low stress levels vL up to higher stress levels vH. This increase is performed at high stress rates and consequently the stress is maintained practically constant for a long period. During this time, the applied stress reaches its maximum value, and the emitted PSC decays gradually and relaxes back to a minimum value. The conducted experiments suggest that the characteristics of the relaxation processes of the PSC depend directly on the high level of the applied stress that is maintained constant after the application of each stress step. Analysis of the macroscopic parameters that characterize the relaxation phenomenon of the PSC provides clear information regarding the proximity of the applied stress to the fracture limit of the rock sample.</p>http://www.annalsofgeophysics.eu/index.php/annals/article/view/5316electric current relaxation phenomena, rock fracture, mechanical stress, PSC, amphibolite
collection DOAJ
language English
format Article
sources DOAJ
author George Hloupis
Ilias Stavrakas
Filippos Vallianatos
Dimos Triantis
spellingShingle George Hloupis
Ilias Stavrakas
Filippos Vallianatos
Dimos Triantis
Relaxation phenomena of electrical signal emissions from rock following application of abrupt mechanical stress
Annals of Geophysics
electric current relaxation phenomena, rock fracture, mechanical stress, PSC, amphibolite
author_facet George Hloupis
Ilias Stavrakas
Filippos Vallianatos
Dimos Triantis
author_sort George Hloupis
title Relaxation phenomena of electrical signal emissions from rock following application of abrupt mechanical stress
title_short Relaxation phenomena of electrical signal emissions from rock following application of abrupt mechanical stress
title_full Relaxation phenomena of electrical signal emissions from rock following application of abrupt mechanical stress
title_fullStr Relaxation phenomena of electrical signal emissions from rock following application of abrupt mechanical stress
title_full_unstemmed Relaxation phenomena of electrical signal emissions from rock following application of abrupt mechanical stress
title_sort relaxation phenomena of electrical signal emissions from rock following application of abrupt mechanical stress
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 2012-04-01
description <p>The emission of electrical signals during application of mechanical stress to brittle geo-materials (the so-called pressure-stimulated current; PSC) can provide significant information regarding the mechanical status of a studied rock sample. PSCs originate as a result of the opening of cracks and microfractures in rock. In this study, such electrical signal emissions are detected and studied when rock samples are subjected to step-wise mechanical stress, increased from low stress levels vL up to higher stress levels vH. This increase is performed at high stress rates and consequently the stress is maintained practically constant for a long period. During this time, the applied stress reaches its maximum value, and the emitted PSC decays gradually and relaxes back to a minimum value. The conducted experiments suggest that the characteristics of the relaxation processes of the PSC depend directly on the high level of the applied stress that is maintained constant after the application of each stress step. Analysis of the macroscopic parameters that characterize the relaxation phenomenon of the PSC provides clear information regarding the proximity of the applied stress to the fracture limit of the rock sample.</p>
topic electric current relaxation phenomena, rock fracture, mechanical stress, PSC, amphibolite
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/5316
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AT iliasstavrakas relaxationphenomenaofelectricalsignalemissionsfromrockfollowingapplicationofabruptmechanicalstress
AT filipposvallianatos relaxationphenomenaofelectricalsignalemissionsfromrockfollowingapplicationofabruptmechanicalstress
AT dimostriantis relaxationphenomenaofelectricalsignalemissionsfromrockfollowingapplicationofabruptmechanicalstress
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