292 research outputs found

    Blowup solutions of Grushin's operator

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    In this note, we consider the blowup phenomenon of Grushin's operator. By using the knowledge of probability, we first get expression of heat kernel of Grushin's operator. Then by using the properties of heat kernel and suitable auxiliary function, we get that the solutions will blow up in finite time.Comment:

    Five types of blow-up in a semilinear fourth-order reaction-diffusion equation: an analytic-numerical approach

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    Five types of blow-up patterns that can occur for the 4th-order semilinear parabolic equation of reaction-diffusion type u_t= -\Delta^2 u + |u|^{p-1} u \quad {in} \quad \ren \times (0,T), p>1, \quad \lim_{t \to T^-}\sup_{x \in \ren} |u(x,t)|= +\iy, are discussed. For the semilinear heat equation ut=Δu+upu_t= \Delta u+ u^p, various blow-up patterns were under scrutiny since 1980s, while the case of higher-order diffusion was studied much less, regardless a wide range of its application.Comment: 41 pages, 27 figure

    Single point gradient blow-up on the boundary for a Hamilton-Jacobi equation with pp-Laplacian diffusion

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    We study the initial-boundary value problem for the Hamilton-Jacobi equation with nonlinear diffusion ut=Δpu+∣∇u∣qu_t=\Delta_p u+|\nabla u|^q in a two-dimensional domain for q>p>2q>p>2. It is known that the spatial derivative of solutions may become unbounded in finite time while the solutions themselves remain bounded. We show that, for suitably localized and monotone initial data, the gradient blow-up occurs at a single point of the boundary. Such a result was known up to now only in the case of linear diffusion (p=2p=2). The analysis in the case p>2p>2 is considerably more delicate

    Blow-up and global existence for the porous medium equation with reaction on a class of Cartan-Hadamard manifolds

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    We consider the porous medium equation with power-type reaction terms upu^p on negatively curved Riemannian manifolds, and solutions corresponding to bounded, nonnegative and compactly supported data. If p>mp>m, small data give rise to global-in-time solutions while solutions associated to large data blow up in finite time. If p<mp<m, large data blow up at worst in infinite time, and under the stronger restriction p∈(1,(1+m)/2]p\in(1,(1+m)/2] all data give rise to solutions existing globally in time, whereas solutions corresponding to large data blow up in infinite time. The results are in several aspects significantly different from the Euclidean ones, as has to be expected since negative curvature is known to give rise to faster diffusion properties of the porous medium equation
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