Disorder in initial porosity triggers persistent channelization at arbitrarily weak levels, whereas erosion-resistance disorder requires a finite strength for a discontinuous transition to localized flow.
Kozeny, Mathematisch Naturwissenschaftliche Abteilung 136, 271 (1927)
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Porosity and Material Disorder Drive Distinct Channelization Transition
Disorder in initial porosity triggers persistent channelization at arbitrarily weak levels, whereas erosion-resistance disorder requires a finite strength for a discontinuous transition to localized flow.