A Barenblatt solution is a mass-preserving source-type similarity solution of the porous medium equation. For the one-dimensional normalizationthe nonnegative profile isIts support is with , and its peak is . Substituting the quadratic profile verifies the partial differential equation wherever it is positive. At the edge, , so extending by zero gives a weak solution without a singular interface flux.
The total mass determines :It is independent of time. As , the support shrinks and the measures converge to , a point source. This is a nonlinear counterpart of the heat kernel, with a finite moving front instead of positive Gaussian tails. The normalization matters: .
For the planar porous medium equation , the mass- point-source similarity solution is , with and . Its front grows as and its central density falls as . The mass conservation integral uses the planar area element . Although the density slope diverges at the front, its diffusion flux vanishes there, giving a compactly supported weak solution with initial measure .
For , the one-dimensional porous medium equation has a volume-preserving similarity solution , where and . On a reflecting half-line with conserved area , , where . For a whole symmetric release use half its total area as . The Beta function fixes normalization, while finite-front zero volume flux fixes the edge condition.
The source-type similarity solution of with whole-line conserved area is , where and . Its volume flux vanishes at the finite front, while the velocity tends to . A reflecting half-line uses twice its prescribed area in these formulas.
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