11 research outputs found

    Error estimates for generalised non-linear Cahn-Hilliard equations on evolving surfaces

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    In this paper, we consider the Cahn--Hilliard equation on evolving surfaces with prescribed velocity and a general non-linear potential which has locally Lipschitz derivatives. High-order evolving surface finite elements are used to discretise the weak equation system in space, and a modified matrix--vector formulation for the semi-discrete problem is derived. The anti-symmetric structure of the equation system is preserved by the spatial discretisation. A new stability proof, based on this structure, combined with consistency bounds proves optimal-order and uniform-in-time error estimates. To demonstrate the advantages of the new stability analysis, an extension of the stability and convergence results is given for generalised non-linear Cahn--Hilliard-type equations on evolving surfaces. The paper is concluded by a variety of numerical experiments

    Short Time Existence for Coupling of Scaled Mean Curvature Flow and Diffusion

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    We prove a short time existence result for a system consisting of a geometric evolution equation for a hypersurface and a parabolic equation on this evolving hypersurface. More precisely, we discuss a mean curvature flow scaled with a term that depends on a quantity defined on the surface coupled to a diffusion equation for that quantity. The proof is based on a splitting ansatz, solving both equations separately using linearization and a contraction argument. Our result is formulated for the case of immersed hypersurfaces and yields a uniform lower bound on the existence time that allows for small changes in the initial value of the height function.Comment: 40 page

    Short time existence for coupling of scaled mean curvature flow and diffusion

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    We prove a short time existence result for a system consisting of a geometric evolution equation for a hypersurface and a parabolic equation on this evolving hypersurface. More precisely, we discuss a mean curvature flow scaled with a term that depends on a quantity defined on the surface coupled to a diffusion equation for that quantity. The proof is based on a splitting ansatz, solving both equations separately using linearization and a contraction argument. Our result is formulated for the case of immersed hypersurfaces and yields a uniform lower bound on the existence time that allows for small changes in the initial value of the height function
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