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On a Hamiltonian PDE arising in magma dynamics
Journal article   Open access   Peer reviewed

On a Hamiltonian PDE arising in magma dynamics

Gideon Simpson, Michael I. Weinstein, Philip Rosenau and Department of Applied Physics and Applied Mathematics, Columbia University, New York, NY 10027
Discrete and continuous dynamical systems. Series B, v 10(4), pp 903-924
01 Nov 2008
url
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.245.2808View
url
https://doi.org/10.3934/dcdsb.2008.10.903View
Published, Version of Record (VoR) Open

Abstract

Mathematics Mathematics, Applied Physical Sciences Science & Technology
In this article we discuss a new Hamiltonian PDE arising from a class of equations appearing in the study of magma, partially molten rock in the Earth's interior. Under physically justifiable simplifications, a scalar, non-linear, degenerate, dispersive wave equation may be derived to describe the evolution of phi, the fraction of molten rock by volume, in the Earth. These equations have two power nonlinearities which specify the constitutive realitions for bulk viscosity and permeability in terms of phi. Previously, they have been shown to admit solitary wave equation to be Hamiltonian; it can be viewed as a generalization of the Benjamin-Bona-Mahoney equation. We prove that the solitary waves are nonlinearly stable, by showing that they are constrained local minimizers of an appropriate time-invariant Lyapunov functional. A consequence is an extension of the regime of global in time well-posedness for this class of equations to (large) data which includes a neighborhood of a solitary traveling waves with compact spatial support.

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Mathematics, Applied
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