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 .
Solved by gpt-5.6-sol high.

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