For and inverse Stefan number , a stagnant mushy-layer model has nearly constant effective heat capacity, giving with . With negligible liquid solutal diffusivity, roof value , positive liquid superheat , and edge , the mush profile is . Matching heat flux requires . The square on in the exponential is essential. The porosity records the leading composition balance; the linear thermal profile is asymptotic, not exact at finite .
Take positive downwards from the roof. Write , , and . The cooled magma follows the decreasing liquidus from towards ; the initially superheated liquid starts at above that liquidus. The solid has zero solute concentration. At each temperature in the mushy layer, a horizontal tie line joins the pure solid to the residual liquid on the liquidus. The lever rule gives the liquid fraction from the bulk concentration. Since , this path stops before the eutectic temperature and does not cross the eutectic composition.
Figure 1.
Liquid cooling, residual-liquid enrichment and a solid–liquid tie line in the stagnant magma mush
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The porosity denotes the liquid fraction, so is the solid fraction. Equal phase mass densities remove volume-change flow; the stable density stratification suppresses convection. In the stagnant mushy-layer model, define bulk specific enthalpy and bulk solute concentration by
The arbitrary reference of specific enthalpy has been omitted. The two conservation laws in are
Here is the thermal diffusivity, with the thermal conductivity. The positive term records increased specific enthalpy on melting; during freezing it supplies latent heat. In the liquid , the heat equation and solute diffusion equation are
where is the solutal diffusivity. Neglecting solute diffusion inside the mushy layer does not permit dropping in the liquid at this stage.
Use , liquid and as , and initially , , for . These are the half-space boundary conditions appropriate before cooling reaches the bottom of the chamber. For a closed chamber of finite depth , replace the far-field conditions by the specified bottom conditions, for example at an insulated impermeable floor; the half-space similarity solution then ceases to apply when the thermal penetration depth approaches .
At , let and be the common liquid concentration and temperature, and let be the limiting porosity on the mush side. Continuity of , the Rankine-Hugoniot condition for solute, and the interfacial conservation of energy give
The first condition has the sign of solute rejection into the liquid. For the sharp-edge stagnant mushy-layer model with nonzero liquid solutal diffusivity, close the free-boundary problem by marginal equilibrium at a mush-liquid boundary:
This prevents constitutional supercooling immediately ahead of the mushy layer. A small solid fraction jump at its edge is allowed: imposing as well as these finite- conditions would generally overdetermine the reduced model. At the roof, follows from the liquidus, and no additional solute-flux boundary condition is needed in the diffusion-free mush.
To obtain the large-concentration similarity solution, put
The positive superheat specifies the physically intended liquid initial state. On a similarity solution, are constant, so every newly incorporated level leaves the same constant . Write and . Then throughout the mushy layer
For , , and , the effective heat capacity is constant to relative error . Thus set
Integration of the similarity solution ordinary differential equation gives the leading analytical profiles
The temperature is . In the mushy layer, the concentration and porosity are the displayed ; in the liquid,
These retain the liquid solutal boundary layer. For completeness, finite- values of are determined analytically, to the same large- order, by setting
and solving
The solute jump gives exactly; replacing by on the right of the last equation retains that jump's next-order factor, but does not make the linearized thermal profiles exact at finite . The branch has , . All these profiles are leading asymptotic expressions, not exact solutions of the nonlinear finite- heat equation.
For at fixed positive , the complementary error function asymptotic gives , hence , , , and . The result simplifies to
In particular, and . There is no finite interfacial latent heat jump in this limit: the latent heat is released continuously throughout the mushy layer. Matching the two temperature gradients gives
The printed final equation is missing the square on in the exponential. The corrected exponent follows directly from differentiating and is consistent with . The positive root is unique: the mush-side gradient decreases from infinity to zero with , whereas increases. The zero-superheat limit is singular and is not described by a finite positive in this two-region construction.