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Statistical similarity between the compression of a porous material and earthquakes

dc.contributor.authorBaró, Jordi
dc.contributor.authorCorral, Alvaro
dc.contributor.authorIlla, Xavier
dc.contributor.authorPlanes, Antoni
dc.contributor.authorSalje, Ekhard K. H.
dc.contributor.authorSchranz, Wilfried
dc.contributor.authorSoto-Parra, Daniel Enrique
dc.contributor.authorVives, Eduard
dc.contributor.editorAmerican Physical Society
dc.date.accessioned2018-04-03T19:23:26Z
dc.date.available2018-04-03T19:23:26Z
dc.date.issued2013-02
dc.identifier.citationBaro, J., Corral, A., Illa, X., et al. (2013). Statistical Similarity between the Compression of a Porous Material and Earthquakes. Physical Review Letters, 110, 088702. ©2013 American Physical Society
dc.identifier.urihttp://hdl.handle.net/11627/3804
dc.description.abstract"It has long been stated that there are profound analogies between fracture experiments and earthquakes; however, few works attempt a complete characterization of the parallels between these so separate phenomena. We study the acoustic emission events produced during the compression of Vycor (SiO2). The Gutenberg-Richter law, the modified Omori's law, and the law of aftershock productivity hold for a minimum of 5 decades, are independent of the compression rate, and keep stationary for all the duration of the experiments. The waiting-time distribution fulfills a unified scaling law with a power-law exponent close to 2.45 for long times, which is explained in terms of the temporal variations of the activity rate."
dc.rightsAttribution-NonCommercial-NoDerivatives 4.0 Internacional
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.subject.classificationFÍSICA
dc.titleStatistical similarity between the compression of a porous material and earthquakes
dc.typearticle
dc.identifier.doihttps://doi.org/10.1103/PhysRevLett.110.088702
dc.rights.accessAcceso Abierto


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