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We study the slow generation
of crack networks as a problem of pattern formation. Issues of pattern selection
and the associated statistical properties are addressed. A typical situation involves the nucleation and propagation of cracks in an overlayer on a frictional substrate. Competition between stress concentration at crack tips and pinning effect by friction leads to a cellular, hierarchical pattern of cracks. Such patterns have a morphology apparently insensitive to the length scales of the system and the microscopic properties of the material--they all "look" the similar, from microns to kms. |
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In a nutshell, we believe that this symmetry-breaking fracturing mode arises by the following mechanism[1], illustrated in the cartoon below: Progressive drying leads to a gradient of stresses across the thickness, as a result the layer folds up and detaches from the substrate, with a front shrinking in time (red circle below). Since stresses are concentrated around the front, when a crack is nucleated it tends to run along the front, giving rise to a spiral. Fittings of experimental and simulation data show that the spirals are logarithmic[2], corresponding to constant angular deviation from a circular crack path. We show that this occurs generally when the crack speed is proportional to the propagating speed of stress front. |
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In a seashell (nautilus and ammonites), logarithmic spirals are ubiquitous albeit formed by an entirely different mechanism. |
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Last updated
October 11, 2002
©KtL
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