2010
DOI: 10.1103/physreve.82.046115
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Scaling in temporal occurrence of quasi-rigid-body vibration pulses due to macrofractures

Abstract: We subjected the time series of quasi-rigid-body vibration pulses (elastic emissions) from laboratory fracture carried out by a piezoelectric accelerometer on concrete and rock specimens under uniaxial compression to statistical analysis. In both cases, we find that the waiting-time distribution can be described by a scaling law extending over several orders of magnitude. This law is indistinguishable from a universal scaling law recently proposed for the waiting-time distributions of acoustic emissions in het… Show more

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Cited by 24 publications
(12 citation statements)
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“…Earthquakes and the collapse of porous materials are related phenomena deeply connected by the emission of crackling noise Salje and Dahmen 2014;Sethna et al 2001) where systems under slow perturbation respond through discrete events, so-called "jerks," with a huge variety of sizes and energies. The signatures of seismic events in geophysics coincide with laboratory-scale experiments ("labquakes") of compressed porous and fractured materials (Davidsen et al 2007;Diodati et al 1991;Hirata 1987;Kun et al 2007Kun et al , 2009Lebyodkin et al 2013;Nataf et al 2014a;Niccolini et al 2009Niccolini et al , 2010Niccolini et al , 2011Petri et al 1994;Salje et al 2013;Weiss and Miguel 2004) and have been simulated by numerical discrete element calculations of porous materials (Kun et al 2013(Kun et al , 2014. In laboratory experiments, external loading is applied to the samples and the system's response is obtained by recording acoustic emission (AE).…”
Section: Introductionmentioning
confidence: 89%
“…Earthquakes and the collapse of porous materials are related phenomena deeply connected by the emission of crackling noise Salje and Dahmen 2014;Sethna et al 2001) where systems under slow perturbation respond through discrete events, so-called "jerks," with a huge variety of sizes and energies. The signatures of seismic events in geophysics coincide with laboratory-scale experiments ("labquakes") of compressed porous and fractured materials (Davidsen et al 2007;Diodati et al 1991;Hirata 1987;Kun et al 2007Kun et al , 2009Lebyodkin et al 2013;Nataf et al 2014a;Niccolini et al 2009Niccolini et al , 2010Niccolini et al , 2011Petri et al 1994;Salje et al 2013;Weiss and Miguel 2004) and have been simulated by numerical discrete element calculations of porous materials (Kun et al 2013(Kun et al , 2014. In laboratory experiments, external loading is applied to the samples and the system's response is obtained by recording acoustic emission (AE).…”
Section: Introductionmentioning
confidence: 89%
“…The tests were carried out at the Laboratory of Fracture Mechanics of the Politecnico di Torino, Italy. By subjecting quasi-brittle materials such as granitic rocks to compression tests, for the first time, bursts of neutron emission (NE) during the failure process were observed [1][2][3][4][5], necessarily involving nuclear reactions, besides the well-known acoustic emission (AE) [6][7][8][9][10][11][12][13], and the phenomenon of electromagnetic radiation (EM) [14][15][16][17][18][19], which is highly suggestive of charge redistribution during material failure and at present under investigation.…”
Section: Introductionmentioning
confidence: 99%
“…While the mechanism of AE is fully understood, being provided by transient elastic waves due to stress redistribution following fracture propagation [6][7][8][9][10][11][12][13], the origin of EME from fracture is not completely clear and different attempts have been made to explain it.…”
Section: Introductionmentioning
confidence: 99%
“…89.75.Da, 62.20.mt, Earthquakes and fractures of materials are phenomena deeply connected under the crackling noise idea [1,2], in which systems under slow perturbation respond through discrete events with a huge variety of sizes. The most fundamental seismic laws also emerge in laboratory-scale experiments related to the fracture of materials [3][4][5][6][7][8][9][10][11][12][13][14][15][16] and have been recently reproduced by numerical discrete element simulations of porous materials [17,18]. In these experiments, an external and constant loading is applied to the material and the system' response is usually obtained by recording acoustic emissions.…”
mentioning
confidence: 99%