Temperature-Induced Explosive Behaviour and Thermo-Chemical Damage on Pyrite-Bearing Limestones: Causes and Mechanisms

Please use this identifier to cite or link to this item: http://hdl.handle.net/10045/109965
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dc.contributorPetrología Aplicadaes_ES
dc.contributorIngeniería del Terreno y sus Estructuras (InTerEs)es_ES
dc.contributor.authorMartínez-Ibáñez, Víctor-
dc.contributor.authorBenavente, David-
dc.contributor.authorHidalgo Signes, Carlos-
dc.contributor.authorTomás, Roberto-
dc.contributor.authorGarrido, M. Elvira-
dc.contributor.otherUniversidad de Alicante. Departamento de Ciencias de la Tierra y del Medio Ambientees_ES
dc.contributor.otherUniversidad de Alicante. Departamento de Ingeniería Civiles_ES
dc.date.accessioned2020-10-29T12:46:58Z-
dc.date.available2020-10-29T12:46:58Z-
dc.date.issued2020-10-28-
dc.identifier.citationRock Mechanics and Rock Engineering. 2021, 54: 219-234. https://doi.org/10.1007/s00603-020-02278-xes_ES
dc.identifier.issn0723-2632 (Print)-
dc.identifier.issn1434-453X (Online)-
dc.identifier.urihttp://hdl.handle.net/10045/109965-
dc.description.abstractIn this investigation, two different varieties of ‘Prada’ limestones were studied: a dark grey texture, bearing quartz, clay minerals, organic matter and pyrites, and a light grey texture with little or no presence of such components. We have observed two effects of different intensity when heating the dark texture from 400 °C: (1) the explosion of certain samples and (2) greater thermal damage than in the light grey texture. Chemical and mineralogical composition, texture, microstructure, and physical properties (i.e. colour, open porosity, P and S-wave velocity) have been evaluated at temperatures of 105, 300, 400, and 500 °C in order to identify differences between textures. The violence of the explosive events was clear and cannot be confounded with ordinary splitting and cracking on thermally treated rocks: exploded samples underwent a total loss of integrity, displacing and overturning the surrounding samples, and embedding fragments in the walls of the furnace, whose impacts were clearly heard in the laboratory. Thermogravimetric results allowed the identification of a process of oxidation of pyrites releasing SO2 from 400 °C. This process jointly with the presence of microfissures in the dark texture, would cause a dramatic increase in pore pressure, leading to a rapid growth and coalescence of microcracks that leads to a process of catastrophic decay in rock integrity. In addition to the explosive events, average ultrasound velocities and open porosity showed a greater variation in the dark grey texture from 400 °C. That result also points towards a significant contribution of oxidation of pyrites on the thermo-chemical damage of the rock, among other factors such as the pre-existence of microfissures and the thermal expansion coefficient mismatch between minerals. Implications in underground infrastructure and mining engineering works are critical, as the explosive potential of pyrite-bearing limestones bears risk for mass fracturing and dramatic strength decay from 400 °C. Moreover, SO2 released has harmful effects on health of people and the potential to form acid compounds that corrode materials, shortening their durability and increasing maintenance costs.es_ES
dc.description.sponsorshipThis work was supported by the Spanish Government [Grant number RTI2018-099052-B-I00] and by the Department of Geological and Geotechnical Engineering, Universitat Politècnica de València.es_ES
dc.languageenges_ES
dc.publisherSpringer Naturees_ES
dc.rights© Springer-Verlag GmbH Austria, part of Springer Nature 2020es_ES
dc.subjectLimestonees_ES
dc.subjectPyrite oxidationes_ES
dc.subjectThermal treatmentes_ES
dc.subjectExplosive behavioures_ES
dc.subjectThermo-chemical damagees_ES
dc.subject.otherPetrología y Geoquímicaes_ES
dc.subject.otherIngeniería del Terrenoes_ES
dc.titleTemperature-Induced Explosive Behaviour and Thermo-Chemical Damage on Pyrite-Bearing Limestones: Causes and Mechanismses_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.peerreviewedsies_ES
dc.identifier.doi10.1007/s00603-020-02278-x-
dc.relation.publisherversionhttps://doi.org/10.1007/s00603-020-02278-xes_ES
dc.identifier.cvIDA10281037-
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES
dc.relation.projectIDinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2017-2020/RTI2018-099052-B-I00-
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