Εμφάνιση απλής εγγραφής

dc.contributor.author Τριάντης, Δήμος Α. el
dc.contributor.author Βαλλιανάτος, Φίλιππος el
dc.contributor.author Σταύρακας, Ηλίας el
dc.contributor.author Χλούπης, Γεώργιος Π. el
dc.date.accessioned 2015-05-16T11:39:04Z
dc.date.available 2015-05-16T11:39:04Z
dc.date.issued 2015-05-16
dc.identifier.uri http://hdl.handle.net/11400/10518
dc.rights Αναφορά Δημιουργού-Μη Εμπορική Χρήση-Όχι Παράγωγα Έργα 3.0 Ηνωμένες Πολιτείες *
dc.rights Αναφορά Δημιουργού-Μη Εμπορική Χρήση-Όχι Παράγωγα Έργα 3.0 Ηνωμένες Πολιτείες *
dc.rights.uri http://creativecommons.org/licenses/by-nc-nd/3.0/us/ *
dc.source http://www.ingv.it/ en
dc.subject Electric current relaxation phenomena
dc.subject Rock fracture
dc.subject mechanical stress
dc.subject PSC
dc.subject Amphibolite
dc.subject Φαινόμενα χαλάρωσης ηλεκτρικού ρεύματος
dc.subject Θραύση βράχου
dc.subject Μηχανική καταπόνηση
dc.subject Αμφιβολίτες
dc.title Relaxation phenomena of electrical signal emissions from rock following application of abrupt mechanical stress en
heal.type journalArticle
heal.classification Technology
heal.classification Electrical engineering
heal.classification Τεχνολογία
heal.classification Ηλεκτρολογία Μηχανολογία
heal.classificationURI http://id.loc.gov/authorities/subjects/sh85133147
heal.classificationURI http://zbw.eu/stw/descriptor/18426-4
heal.classificationURI **N/A**-Τεχνολογία
heal.classificationURI **N/A**-Ηλεκτρολογία Μηχανολογία
heal.keywordURI http://lod.nal.usda.gov/1734
heal.keywordURI http://id.loc.gov/authorities/subjects/sh85004613
heal.identifier.secondary DOI: 10.4401/ag-5316
heal.language en
heal.access campus
heal.publicationDate 2012
heal.bibliographicCitation TRIANTIS, D.A., VALLIANATOS, F., STAVRAKAS, I. & HLOUPIS, G.P. (2012). Relaxation phenomena of electrical signal emissions from rock following application of abrupt mechanical stress. Annals of Geophysics. [Online] 55 (1). p. 207-212. Available from: http://www.ingv.it/ en
heal.abstract 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 σ L up to higher stress levels σ H. 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. en
heal.publisher Istituto Nazionale di Geofisica e Vulcanologia it
heal.journalName Annals of Geophysics en
heal.journalType peer-reviewed
heal.fullTextAvailability true


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Εμφάνιση απλής εγγραφής

Αναφορά Δημιουργού-Μη Εμπορική Χρήση-Όχι Παράγωγα Έργα 3.0 Ηνωμένες Πολιτείες Εκτός από όπου ορίζεται κάτι διαφορετικό, αυτή η άδεια περιγράφεται ως Αναφορά Δημιουργού-Μη Εμπορική Χρήση-Όχι Παράγωγα Έργα 3.0 Ηνωμένες Πολιτείες