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dc.contributor.authorPosadas Chinchilla, Antonio Miguel
dc.contributor.authorMorales Soto, José 
dc.contributor.authorIbáñez Godoy, Jesús Miguel 
dc.contributor.authorPosadas Garzón, A.
dc.date.accessioned2021-10-15T09:56:16Z
dc.date.available2021-10-15T09:56:16Z
dc.date.issued2021-10
dc.identifier.citationPosadas, A., Morales, J., Ibañez, J. M., & Posadas-Garzon, A. (2021). Shaking earth: Non-linear seismic processes and the second law of thermodynamics: A case study from Canterbury (New Zealand) earthquakes. Chaos, Solitons & Fractals, 151, 111243. [https://doi.org/10.1016/j.chaos.2021.111243]es_ES
dc.identifier.urihttp://hdl.handle.net/10481/70879
dc.descriptionWe would like to express our gratitude to GeoNet for making available the data used in this work. This work was partially sup-ported by the RNM104 and RNM194 (Research Groups belonging to Junta de Andalucia, Spain) , the Spanish National Projects [grant project PID2019-109608GB-I00] , and the Junta de Andalucia Project [grant project A-RNM-421-UGR18] . English language editing was performed by Tornillo Scientific.es_ES
dc.description.abstractEarthquakes are non-linear phenomena that are often treated as a chaotic natural processes. We propose the use of the Second Law of Thermodynamics and entropy, H, as an indicator of the equilibrium state of a seismically active region (a seismic system). In this sense, in this paper we demonstrate the exportability of first principles (e.g., thermodynamics laws) to others scientific fields (e.g., seismology). We suggest that the relationship between increasing H and the occurrence of large earthquakes reflects the irreversible transition of a system. From this point of view, a seismic system evolves from an unstable initial state (due to external stresses) to a state of reduced stress after an earthquake. This is an irreversible transition that entails an increase in entropy. In other words, a seismic system is in a metastable situation that can be characterised by the Second Law of Thermodynamics. We investigated two seismic episodes in the Canterbury area of New Zealand: the 2010 Christchurch earthquake (M = 7.2) and the 2016 Kaikoura earthquake (M = 7.8). The results are remarkably in line with our theoretical forecasts. In other words, an earthquake, understood as an irreversible transition, must results in an increase in entropy.es_ES
dc.description.sponsorshipResearch Groups belonging to Junta de Andalucia, Spain RNM104- RNM194es_ES
dc.description.sponsorshipSpanish National Projects PID2019-109608GB-I00es_ES
dc.description.sponsorshipJunta de Andalucia A-RNM-421-UGR18es_ES
dc.language.isoenges_ES
dc.publisherElsevieres_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subjectNonlinear dynamicses_ES
dc.subjectEarthquakeses_ES
dc.subjectSecond law of thermodynamicses_ES
dc.subjectEntropy es_ES
dc.subjectCanterbury earthquakeses_ES
dc.titleShaking earth: Non-linear seismic processes and the second law of thermodynamics: A case study from Canterbury (New Zealand) earthquakeses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.identifier.doi10.1016/j.chaos.2021.111243
dc.type.hasVersioninfo:eu-repo/semantics/publishedVersiones_ES


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