Fick's first law gives the diffusive flux
Local conservation says , and therefore
For , conservation of the deposited amount requires
The dimensions satisfy and . Thus has dimension , so the similarity length is . Requiring the concentration scale to have dimension gives
Hence
In polar coordinates, substitution into
gives
Multiplying by and integrating once, with regularity and zero radial flux at the origin, yields
Where , this reduces to , so
Nonnegativity and zero flux at the moving front give the compactly supported profile
The normalization gives
and hence and . This is the Two-dimensional Barenblatt solution with diffusivity proportional to concentration, and its support radius is
so .
Now add the linear reaction term and write
Substitution cancels the terms and leaves
Choosing
produces , as in the linear-reaction time change for quadratic nonlinear diffusion. Therefore
For , the front grows like while the central concentration decays like . For , , so the front grows like and the central concentration like . For , : the front approaches a finite limiting radius while the concentration decays exponentially to zero.
At times long compared with the encounter time at depth , the fixed depth is negligible relative to the growing diffusion lengths. Salt obeys the diffusion equation with diffusivity . With
the self-similar concentration profile in the liquid is
It has and tends to in the far field.
Because the solid contains no salt, conservation of solute at the moving boundary requires the rejected solute flux from Fick's first law to equal the rate at which the interface sweeps up salt:
Substituting the similarity profile gives
This relation determines if is already known. More generally it must be solved together with the thermal Stefan condition and the interfacial phase-equilibrium relation from the liquidus. For , salt occupies a much thinner boundary layer than heat and can be much larger than .