The porous medium equation, also called the nonlinear heat equation, is a nonlinear partial differential equation taking the form:where Δ {\displaystyle \Delta } is the Laplace operator. It may also be put into its equivalent divergence form: ∂ u ∂ t = ∇ ⋅ [ D ( u ) ∇ u ] {\displaystyle {\partial u \over {\partial t}}=\nabla \cdot \left[D(u)\nabla u\right]} where D ( u ) = m u m − 1 {\displaystyle D(u)=mu^{m-1}} may be interpreted as a diffusion coefficient and ∇ ⋅ ( ⋅ ) {\displaystyle \nabla \cdot (\cdot )} is the divergence operator.
Solutions Despite being a nonlinear equation, the porous medium equation may be solved exactly using separation of variables or a similarity solution. However, the separation of variables solution is known to blow up to infinity at a finite time.
Barenblatt-Kompaneets-Zeldovich similarity solution The similarity approach to solving the porous medium equation was taken by Barenblatt and Kompaneets/Zeldovich, which for x ∈ R n {\displaystyle x\in \mathbb {R} ^{n}} was to find a solution satisfying: u ( t , x ) = 1 t α v ( x t β ) , t > 0 {\displaystyle u(t,x)={1 \over {t^{\alpha }}}v\left({x \over {t^{\beta }}}\right),\quad t>0} for some unknown function v {\displaystyle v} and unknown constants α , β {\displaystyle \alpha ,\beta } . The final solution to the porous medium equation under these scalings is: u ( t , x ) = 1 t α ( b − m − 1 2 m β ‖ x ‖ 2 t 2 β ) + 1 m − 1 {\displaystyle u(t,x)={1 \over {t^{\alpha }}}\left(b-{m-1 \over {2m}}\beta {\|x\|^{2} \over {t^{2\beta }}}\right)_{+}^{1 \over {m-1}}} where ‖ ⋅ ‖ 2 {\displaystyle \|\cdot \|^{2}} is the ℓ 2 {\displaystyle \ell ^{2}} -norm, ( ⋅ ) + {\displaystyle (\cdot )_{+}} is the positive part, and the coefficients are given by: α = n n ( m − 1 ) + 2 , β = 1 n ( m − 1 ) + 2 {\displaystyle \alpha ={n \over {n(m-1)+2}},\quad \beta ={1 \over {n(m-1)+2}}}
Applications The porous medium equation has been found to have a number of applications in gas flow, heat transfer, and groundwater flow.
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