For constant porosity and permeability, the equation is . Under , , , the chain rule gives and . Thus the moving-frame porous medium equation is
Its conserved mass is .
There is a source inconsistency in the printed volume formula. Actual liquid volume is . The stated coordinates have Jacobian determinant
so the volume Jacobian for downslope stretched coordinates requires
The printed factor in the first expression is its reciprocal and cannot be proved with these coordinates. For example, at an integral equal to one corresponds to actual volume , whereas the printed formula gives . The physical-volume normalization below uses the corrected Jacobian.
Let . For the source-type axisymmetric similarity solution, put
Mass conservation imposes , and balancing against gives . Hence and . The profile equation is
Multiplying by , the left side is . Integration and regularity at the origin give
Where , divide by to obtain , so
Set the profile to zero beyond this front. The mass normalization is
Therefore the two-dimensional Barenblatt profile for quadratic porous-medium diffusion is
where . Its radius and central thickness are
The profile is regular at the center, its flux vanishes at the dry edge, and the front speed equals the limiting advective speed there. Its support shrinks to the release point as while its mass stays , giving the concentrated initial release in the weak sense.
In physical coordinates its center travels at
and with . If the printed volume expression were instead adopted merely as a definition of a formal parameter , the same profile would use ; that parameter would equal , not the actual released fluid volume.