2,684 research outputs found

    Corrector estimates for the homogenization of a locally-periodic medium with areas of low and high diffusivity

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    We prove an upper bound for the convergence rate of the homogenization limit ϵ0\epsilon\to 0 for a linear transmission problem for a advection-diffusion(-reaction) system posed in areas with low and high diffusivity, where ϵ\epsilon is a suitable scale parameter. On this way, we justify the formal homogenization asymptotics obtained by us earlier by proving an upper bound for the convergence rate (a corrector estimate). The main ingredients of the proof of the corrector estimate include integral estimates for rapidly oscillating functions with prescribed average, properties of the macroscopic reconstruction operators, energy bounds and extra two-scale regularity estimates. The whole procedure essentially relies on a good understanding of the analysis of the limit two-scale problem.Comment: 19 pages, 1 figur

    D-Jogger: Syncing Music with Walking

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    Homogenization of a locally-periodic medium with areas of low and high diffusivity

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    We aim at understanding transport in porous materials including regions with both high and low diffusivities. For such scenarios, the transport becomes structured (here: micro- macro). The geometry we have in mind includes regions of low diffusivity arranged in a locally-periodic fashion. We choose a prototypical advection-diffusion system (of minimal size), discuss its formal homogenization (the heterogenous medium being now assumed to be made of zones with circular areas of low diffusivity of x-varying sizes), and prove the weak solvability of the limit two-scale reaction-diffusion model. A special feature of our analysis is that most of the basic estimates (positivity, L^inf-bounds, uniqueness, energy inequality) are obtained in x-dependent Bochner spaces. Keywords: Heterogeneous porous materials, homogenization, micro-macro transport, two-scale model, reaction-diffusion system, weak solvability

    A Stefan problem modelling dissolution and precipitation in porous media

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