dc.contributor.author | Baró, Jordi | |
dc.contributor.author | Corral, Alvaro | |
dc.contributor.author | Illa, Xavier | |
dc.contributor.author | Planes, Antoni | |
dc.contributor.author | Salje, Ekhard K. H. | |
dc.contributor.author | Schranz, Wilfried | |
dc.contributor.author | Soto-Parra, Daniel Enrique | |
dc.contributor.author | Vives, Eduard | |
dc.contributor.editor | American Physical Society | |
dc.date.accessioned | 2018-04-03T19:23:26Z | |
dc.date.available | 2018-04-03T19:23:26Z | |
dc.date.issued | 2013-02 | |
dc.identifier.citation | Baro, 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.uri | http://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.rights | Attribution-NonCommercial-NoDerivatives 4.0 Internacional | |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/4.0/ | |
dc.subject.classification | FÍSICA | |
dc.title | Statistical similarity between the compression of a porous material and earthquakes | |
dc.type | article | |
dc.identifier.doi | https://doi.org/10.1103/PhysRevLett.110.088702 | |
dc.rights.access | Acceso Abierto | |