1982
DOI: 10.1016/0031-9201(82)90075-9
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Percolation and fracture

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Cited by 103 publications
(53 citation statements)
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“…As an analogy to the study of critical phase transitions in statistical physics, it has been argued that the fracture of heterogeneous materials could be viewed as a critical phenomenon either at the laboratory scale or at the geophysical scale (Chelidze, 1982;Allegre et al, 1982;Sornette and Sornette, 1990;Herrmann and Roux, 1990;Sornette and Sammis, 1995;Sornette and Andersen, 1998;Bowman et al, 1998;Kossobokov et al, 1999;Sornette, 2000;Moreno, 2000;Gluzman and Sornette, 2001;Guarino et al, 2002;Rundle et al, 2003, and references therein). We note that other researchers have associated brittle rupture with a firstorder phase transition (Buchel and Sethna, 1997;Kun and Herrmann, 1999;Rundle et al, 2003, and references therein).…”
Section: Focus On Mhz Em Fieldmentioning
confidence: 99%
“…As an analogy to the study of critical phase transitions in statistical physics, it has been argued that the fracture of heterogeneous materials could be viewed as a critical phenomenon either at the laboratory scale or at the geophysical scale (Chelidze, 1982;Allegre et al, 1982;Sornette and Sornette, 1990;Herrmann and Roux, 1990;Sornette and Sammis, 1995;Sornette and Andersen, 1998;Bowman et al, 1998;Kossobokov et al, 1999;Sornette, 2000;Moreno, 2000;Gluzman and Sornette, 2001;Guarino et al, 2002;Rundle et al, 2003, and references therein). We note that other researchers have associated brittle rupture with a firstorder phase transition (Buchel and Sethna, 1997;Kun and Herrmann, 1999;Rundle et al, 2003, and references therein).…”
Section: Focus On Mhz Em Fieldmentioning
confidence: 99%
“…In analogy to the study of critical phase transitions in statistical physics, it has been recently argued that the fracture of heterogeneous materials could be viewed as a critical phenomenon (Herrmann and Roux, 1990;Vanneste and Sornette, 1992;Lamaignere et al, 1996;Andersen et al, 1997;Sornette, 2000), either at laboratory scale (Petri et al, 1994;Guarino et al, 1998Guarino et al, , 2002 or at geophysical scales (Chelidze, 1982;Allegre et al, 1982;Sornette and Sornette, 1990;Diodati et al, 1991;Sornette and Sammis, 1995;Saleur et al, 1996a,b;Main, 1996;Bowman et al, 1998;Kossobokov et al, 1999). This result comes from different observations including power law scaling in space (fractals), time and energy, long-range correlations, or the divergence of the rate of energy dissipation near the critical point.…”
Section: Introductionmentioning
confidence: 99%
“…Faults are generated by large-scale tectonic events, and joints by uplift and erosion, excess fluid pressures, and ther- Largely because of data uncertainty, and lack of distinction between faults and joints, there has been considerable debate whether available fracture network measurements, and understanding of fracturing mechanisms, suggest fractures in the Earth to be well above the percolation threshold, and highly interconnected [Barton, 1995], or, conversely, near the percolation threshold and thus poorly connected [Chelidze, 1982;Madden, 1983 With the length distribution being fixed, we examine the critical percolation parameter, P•, which we define as the threshold at which a network has a connection probability across the domain of 0.5. Standard percolation theory concepts hold only for random placements of constant length bonds, or for distributions of bond lengths which are significantly smaller than the domain size.…”
Section: Introductionmentioning
confidence: 99%