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Titlebook: Non-Linearity and Breakdown in Soft Condensed Matter; Proceedings of a Wor Kamal K. Bardhan,Bikas K. Chakrabarti,Alex Hansen Conference pro

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0075-8450 t a mesoscopic scale, where local disorder and nonlinearity influence the global behaviour of cracks, for example, and problems where randomness in time evolution is as crucial as the geometry itself.978-3-662-13958-5978-3-540-49037-1Series ISSN 0075-8450 Series E-ISSN 1616-6361
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Pattern formation in particulate complex fluids: A guided tour,iar flow or fracture behaviors which allows for a rich variety of fractal patterns, including viscous fingers, viscoelastic fracturing patterns, rough fracture surfaces, and granular displacement patterns.
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Fracture roughness and physical implications, some physical consequences of this property. The examples we consider concern the permeability of a crack, a percolation transition through long-range correlated surfaces, the elastic contact between two rough surfaces, and a simple model of dynamic friction.
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Decompaction, fluidisation and segregation in a 2D sandpile,he whole range of behaviour of common dry particulates such as sand : Spontaneous heaping, size segregation , convection, surface fluidisation etc. Modelling sand with a 2D set of particles has the crucial advantage of allowing a direct observation of the interplay of these processes, as well as all
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Density waves in granular flow,r Dynamics Simulations we show that several types of waves exist and find that these density fluctuations follow a 1/. spectrum. We compare this behaviour to deterministic one-dimensional traffic models. If positions and velocities are continuous variables the model shows self-organized criticality
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Height fluctuations and pressure distribution in a model of random close packing of mono-size discse the correlation function of the fluctuations of the height in the .-th layer, and show that the width varies as .. for large n. Assuming that the discs are frictionless we calculate the pressure distribution at the floor and show that the pressure distribution is uniform and is independent of the
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