# Nonlocal porous medium equation

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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]]. | 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 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: any nontrivial nonnegative solution becomes strictly positive instantaneously. |

- | This means that the first model presents us with a [[free boundary problem]]. For this model global existence and Hölder continuity of weak solutions have been | + | This means that the first model presents us with a [[free boundary problem]]. For this model global existence and Hölder continuity of weak solutions have been obtained <ref name="CV1"/>. The properties of its free boundary are less well understood. In the one-dimensional case, this equation is equivalent to a model for the [[dislocation dynamics | dynamics of dislocation lines]]. In this case, the uniqueness of solutions has been obtained <ref name="BMK"/>. Uniqueness is still unknown in higher dimensions. |

- | For the second equation, | + | For the second equation, the Cauchy problem, the regularity of solutions and long time behavior, have been extensively studied in recent years <ref name="PQRV" />. |

== References == | == References == |

## Latest revision as of 02:48, 16 April 2015

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: any nontrivial nonnegative solution becomes strictly positive instantaneously.

This means that the first model presents us with a free boundary problem. For this model global existence and Hölder continuity of weak solutions have been obtained ^{[1]}. The properties of its free boundary are less well understood. In the one-dimensional case, this equation is equivalent to a model for the dynamics of dislocation lines. In this case, the uniqueness of solutions has been obtained ^{[2]}. Uniqueness is still unknown in higher dimensions.

For the second equation, the Cauchy problem, the regularity of solutions and long time behavior, have been extensively studied in recent years ^{[3]}.

## References

- ↑ Caffarelli, Luis; Vazquez, Juan (2011), "Nonlinear Porous Medium Flow with Fractional Potential Pressure",
*Archive for Rational Mechanics and Analysis*(Springer Berlin / Heidelberg): 1–29, ISSN 0003-9527, http://dx.doi.org/10.1007/s00205-011-0420-4 - ↑ Biler, Piotr; Monneau, Régis; Karch, Grzegorz (2009), "Nonlinear Diffusion of Dislocation Density and Self-Similar Solutions",
*Communications in Mathematical Physics***294**(1): 145–168, doi:10.1007/s00220-009-0855-8, ISSN 0010-3616 - ↑ Pablo, Arturo de; Quirós, Fernando; Rodríguez, Ana; Vazquez, Juan Luis (2011), "A fractional porous medium equation",
*Advances in Mathematics***226**(2): 1378–1409, doi:DOI: 10.1016/j.aim.2010.07.017, ISSN 0001-8708, http://www.sciencedirect.com/science/article/pii/S0001870810003130