Avalanches in compressed porous SiO2-based materials

Guillaume F. Nataf, Pedro O. Castillo-Villa, Jordi Baró, Xavier Illa, Eduard Vives, Antoni Planes, and Ekhard K. H. Salje
Phys. Rev. E 90, 022405 – Published 15 August 2014

Abstract

The failure dynamics in SiO2-based porous materials under compression, namely the synthetic glass Gelsil and three natural sandstones, has been studied for slowly increasing compressive uniaxial stress with rates between 0.2 and 2.8 kPa/s. The measured collapsed dynamics is similar to Vycor, which is another synthetic porous SiO2 glass similar to Gelsil but with a different porous mesostructure. Compression occurs by jerks of strain release and a major collapse at the failure point. The acoustic emission and shrinking of the samples during jerks are measured and analyzed. The energy of acoustic emission events, its duration, and waiting times between events show that the failure process follows avalanche criticality with power law statistics over ca. 4 decades with a power law exponent ɛ 1.4 for the energy distribution. This exponent is consistent with the mean-field value for the collapse of granular media. Besides the absence of length, energy, and time scales, we demonstrate the existence of aftershock correlations during the failure process.

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  • Received 23 May 2014
  • Corrected 21 August 2014

DOI:https://doi.org/10.1103/PhysRevE.90.022405

©2014 American Physical Society

Corrections

21 August 2014

Erratum

Publisher's Note: Avalanches in compressed porous SiO2-based materials [Phys. Rev. E 90, 022405 (2014)]

Guillaume F. Nataf, Pedro O. Castillo-Villa, Jordi Baró, Xavier Illa, Eduard Vives, Antoni Planes, and Ekhard K. H. Salje
Phys. Rev. E 90, 029904 (2014)

Authors & Affiliations

Guillaume F. Nataf

  • Departament d'Estructura i Constituents de la Matèria, Facultat de Física, Universitat de Barcelona, Diagonal 647, E-08028 Barcelona, Catalonia, and INP Grenoble, 38031 Grenoble Cedex 1, France

Pedro O. Castillo-Villa, Jordi Baró, Xavier Illa, Eduard Vives, and Antoni Planes

  • Departament d'Estructura i Constituents de la Matèria, Facultat de Física, Universitat de Barcelona, Diagonal 647, E-08028 Barcelona, Catalonia

Ekhard K. H. Salje

  • Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, United Kingdom

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Issue

Vol. 90, Iss. 2 — August 2014

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