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- W2079595003 abstract "A modification to the renormalization group approach of Allègre et al. (1982) and Turcotte (1986) is developed for ice. This yields the fractal dimension of 2.42, compared to 2.5 observed by Timco and Jordaan (1987) for the distribution of crushed mass as a function of fragment size, M∝r−D, where M is the mass of fragments with linear dimension greater than r. In Allègre et al. (1982) “pillars of soundenss” were used a models of fragility and D = 2.84 was obtained. Turcotte (1986) used “planes of weakness” as the fragility criteria and obtained D = 1.97. By prohibiting failure along one orientation of cracks in ice, and reducing the number of fragile configurations in the “plane of weakness model”, a value of D = 2.42 is obtained. This is in much better agreement with observation." @default.
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- W2079595003 date "1991-11-01" @default.
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- W2079595003 title "A renormalized group model for the fragmentation of ice" @default.
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- W2079595003 doi "https://doi.org/10.1016/0165-232x(91)90059-p" @default.
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