195 research outputs found

    The parabolic-parabolic Keller-Segel system with critical diffusion as a gradient flow in \RR^d, d≄3d \ge 3

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    It is known that, for the parabolic-elliptic Keller-Segel system with critical porous-medium diffusion in dimension \RR^d, d≄3d \ge 3 (also referred to as the quasilinear Smoluchowski-Poisson equation), there is a critical value of the chemotactic sensitivity (measuring in some sense the strength of the drift term) above which there are solutions blowing up in finite time and below which all solutions are global in time. This global existence result is shown to remain true for the parabolic-parabolic Keller-Segel system with critical porous-medium type diffusion in dimension \RR^d, d≄3d \ge 3, when the chemotactic sensitivity is below the same critical value. The solution is constructed by using a minimising scheme involving the Kantorovich-Wasserstein metric for the first component and the L2L^2-norm for the second component. The cornerstone of the proof is the derivation of additional estimates which relies on a generalisation to a non-monotone functional of a method due to Matthes, McCann, & Savar\'e (2009)

    Finite time blow-up for radially symmetric solutions to a critical quasilinear Smoluchowski-Poisson system

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    Finite time blow-up is shown to occur for radially symmetric solutions to a critical quasilinear Smoluchowski-Poisson system provided that the mass of the initial condition exceeds an explicit threshold. In the supercritical case, blow-up is shown to take place for any positive mass. The proof relies on a novel identity of virial type

    Asymptotic behavior for a viscous Hamilton-Jacobi equation with critical exponent

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    The large time behavior of non-negative solutions to the viscous Hamilton-Jacobi equation ut−Δu+∣∇u∣q=0u_t - \Delta u + |\nabla u|^q = 0 in the whole space RNR^N is investigated for the critical exponent q=(N+2)/(N+1)q = (N+2)/(N+1). Convergence towards a rescaled self-similar solution of the linear heat equation is shown, the rescaling factor being (log⁡(t))−(N+1)(\log(t))^{-(N+1)}. The proof relies on the construction of a one-dimensional invariant manifold for a suitable truncation of the equation written in self-similar variables.Comment: 17 pages, no figur

    On an age and spatially structured population model for Proteus Mirabilis swarm-colony development

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    Proteus mirabilis are bacteria that make strikingly regular spatial-temporal patterns on agar surfaces. In this paper we investigate a mathematical model that has been shown to display these structures when solved numerically. The model consists of an ordinary differential equation coupled with a partial differential equation involving a first-order hyperbolic aging term together with nonlinear degenerate diffusion. The system is shown to admit global weak solutions

    Weak solutions to the continuous coagulation equation with multiple fragmentation

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    The existence of weak solutions to the continuous coagulation equation with multiple fragmentation is shown for a class of unbounded coagulation and fragmentation kernels, the fragmentation kernel having possibly a singularity at the origin. This result extends previous ones where either boundedness of the coagulation kernel or no singularity at the origin for the fragmentation kernel were assumed

    Global existence for a hydrogen storage model with full energy balance

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    A thermo-mechanical model describing hydrogen storage by use of metal hydrides has been recently proposed in a paper by Bonetti, Fr\'emond and Lexcellent. It describes the formation of hydrides using the phase transition approach. By virtue of the laws of continuum thermo-mechanics, the model leads to a phase transition problem in terms of three state variables: the temperature, the phase parameter representing the fraction of one solid phase, and the pressure, and is derived within a generalization of the principle of virtual powers proposed by Fr\'emond accounting for micro-forces, responsible for the phase transition, in the whole energy balance of the system. Three coupled nonlinear partial differential equations combined with initial and boundary conditions have to be solved. The main difficulty in investigating the resulting system of partial differential equations relies on the presence of the squared time derivative of the order parameter in the energy balance equation. Here, the global existence of a solution to the full problem is proved by exploiting known and sharp estimates on parabolic equations with right hand side in L^1. Some complementary results on stability and steady state solutions are also given.Comment: Key-words: phase transition model; hydrogen storage; nonlinear parabolic system; existenc
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