A mushy layer contains solid crystals and liquid in local phase equilibrium, rather than a single sharp phase boundary. Its solid fraction changes as heat and solute are transported. A concentration-dependent liquidus couples temperature to liquid composition; a connected crystal framework makes the residual liquid behave as a porous-media flow.
The solid fraction is the volume fraction occupied by solid in a solid–liquid mixture. The complementary liquid fraction is .
The liquid fraction is the volume fraction occupied by liquid in a solid–liquid mixture. For a saturated rigid mushy layer, it is the porosity available to Darcy flux.
For constant phase mass densities , a fixed solid framework has mixture density . Mass conservation giveswhere is Darcy flux. Equal phase densities give a divergence-free flux. Unequal densities require expansion or contraction flow during freezing or melting.
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