# Nonlocal porous medium equation

(Difference between revisions)
 Revision as of 06:37, 2 June 2011 (view source)Nestor (Talk | contribs) (Created page with "The nonlocal porous medium equation of order $\sigma$ is the name currently given to two very different equations, namely $u_t = \nabla \cdot \left ( u \nabla \mathcal{K_\alph...")← Older edit Revision as of 06:42, 2 June 2011 (view source)Nestor (Talk | contribs) Newer edit → Line 9: Line 9: \[ u_t +(-\Delta)^{s}(u^m) = 0$ $u_t +(-\Delta)^{s}(u^m) = 0$ - These equations agree when $s=1$ and $m=2$. They are fractional order [[Quasilinear equations]]. + These equations agree when $s=1$ and $m=2$, otherwise they are not only different superficially, they also exhibit extremely different behaviors. They are both fractional order [[Quasilinear equations]]. The first of the two has the remarkable property (for nonlocal equations at least) that any initial data with compact support remains with compact support for all later times, the opposite is true of the second equation, for which [[instantaneous speed of propagation]] holds, thus, at least from the point of view of [[free boundary problems]], the first equation is the "truer" nonlocal porous medium equation. + + + + [[Categories:Quasilinear equations]] [[Categories:Evolution equations]] [[Categories:Free boundary problems]]

## Revision as of 06:42, 2 June 2011

The nonlocal porous medium equation of order $\sigma$ is the name currently given to two very different equations, namely

$u_t = \nabla \cdot \left ( u \nabla \mathcal{K_\alpha} (u) \right )$

$\mbox{ where } \mathcal{K}_\alpha(u) := C_{n,\alpha}\; u * |x|^{-n+\alpha},\;\; \alpha+2=\sigma$

and

$u_t +(-\Delta)^{s}(u^m) = 0$

These equations agree when $s=1$ and $m=2$, otherwise they are not only different superficially, they also exhibit extremely different behaviors. They are both fractional order Quasilinear equations. The first of the two has the remarkable property (for nonlocal equations at least) that any initial data with compact support remains with compact support for all later times, the opposite is true of the second equation, for which instantaneous speed of propagation holds, thus, at least from the point of view of free boundary problems, the first equation is the "truer" nonlocal porous medium equation.