arXiv · 1212.1129
Gradient flow structures for discrete porous medium equations
Abstract
We consider discrete porous medium equations of the form \partial_t \rho_t = \Delta \phi(\rho_t), where \Delta is the generator of a reversible continuous time Markov chain on a finite set X, and \phi is an increasing function. We show that these equations arise as gradient flows of certain entropy functionals with respect to suitable non-local transportation metrics. This may be seen as a discrete analogue of the Wasserstein gradient flow structure for porous medium equations in R^n discovered by Otto. We present a one-dimensional counterexample to geodesic convexity and discuss Gromov-Hausdorff convergence to the Wasserstein metric.
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Matthias Erbar, Jan Maas. 2012-12-05. Gradient flow structures for discrete porous medium equations. https://arxiv.org/abs/1212.1129
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