Quasilinear equations: Difference between revisions
imported>Luis No edit summary |
imported>Luis No edit summary |
||
Line 3: | Line 3: | ||
For instance, the following equations are all quasilinear (and the first two are NOT semilinear) | For instance, the following equations are all quasilinear (and the first two are NOT semilinear) | ||
=== Mean curvature flow === | |||
\[u_t-\mbox{div} \left ( \frac{\nabla u}{\sqrt{1+|\nabla u|^2}}\right ) = 0 \] | \[u_t-\mbox{div} \left ( \frac{\nabla u}{\sqrt{1+|\nabla u|^2}}\right ) = 0 \] | ||
=== [[Nonlocal porous medium equation]] === | |||
\[ u_t = \mbox{div} \left ( u \nabla \mathcal{K_\alpha} u\right ),\;\;\; \mathcal{K_\alpha} u = u * |x|^{-n+\alpha} \] | \[ u_t = \mbox{div} \left ( u \nabla \mathcal{K_\alpha} u\right ),\;\;\; \mathcal{K_\alpha} u = u * |x|^{-n+\alpha} \] | ||
=== [[Semilinear equations|Hamilton-Jacobi with fractional diffusion]] === | |||
\[ u_t + (-\Delta)^s u + H(x,t,u,\nabla u)= 0.\] | \[ u_t + (-\Delta)^s u + H(x,t,u,\nabla u)= 0.\] | ||
Equations which are NOT quasilinear, and thus involve no linearity assumption of any sort, are called [[Fully nonlinear equations]], they include for instance the [[Monge Ampére Equation]] and [[Fully nonlinear integro-differential equations]]. Note that all [[Semilinear equations]] are automatically quasilinear. | Equations which are NOT quasilinear, and thus involve no linearity assumption of any sort, are called [[Fully nonlinear equations]], they include for instance the [[Monge Ampére Equation]] and [[Fully nonlinear integro-differential equations]]. Note that all [[Semilinear equations]] are automatically quasilinear. |
Latest revision as of 20:40, 15 April 2015
Quasilinear equations are those which are linear in all terms except for the highest order derivatives (whether they are of fractional order or not).
For instance, the following equations are all quasilinear (and the first two are NOT semilinear)
Mean curvature flow
\[u_t-\mbox{div} \left ( \frac{\nabla u}{\sqrt{1+|\nabla u|^2}}\right ) = 0 \]
Nonlocal porous medium equation
\[ u_t = \mbox{div} \left ( u \nabla \mathcal{K_\alpha} u\right ),\;\;\; \mathcal{K_\alpha} u = u * |x|^{-n+\alpha} \]
Hamilton-Jacobi with fractional diffusion
\[ u_t + (-\Delta)^s u + H(x,t,u,\nabla u)= 0.\]
Equations which are NOT quasilinear, and thus involve no linearity assumption of any sort, are called Fully nonlinear equations, they include for instance the Monge Ampére Equation and Fully nonlinear integro-differential equations. Note that all Semilinear equations are automatically quasilinear.
This article is a stub. You can help this nonlocal wiki by expanding it.