Let
The Neumann solution of the Stefan problem in the ice and substrate is
and
Continuity of heat flux at the contact gives, with ,
and therefore
At the ice–water interface, the water is isothermal at . The Stefan condition gives
Eliminating yields the implicit equation
which determines and hence .
If , then , , and
The highly conducting substrate acts as a reservoir fixed near its initial cold temperature, giving the usual one-phase Stefan problem.
If , then , , and . Consequently
Here heat removal through the poorly conducting substrate is rate limiting, and only a small temperature drop is needed across the much more conducting ice.
Measure upward from the heat exchanger and let the steady ice front be at . In the exchanger frame, salt in the liquid satisfies the advection-diffusion equation
The decaying solution and the prescribed total salt mass are
so
The linear liquidus condition fixes the interface temperature as
A solid layer between the exchanger and the interface can therefore exist only if
Write . Heat advection, conduction, and environmental loss give
Its characteristic exponents are
Below the exchanger and above the ice front, boundedness gives
In , the ice temperature is
where
Substitution of these fields into the Stefan condition
gives one scalar equation for the steady height , which can be solved numerically. The heat flux may jump at because the exchanger supplies the required localized cooling.
The local equilibrium freezing temperature ahead of the front is
Because , constitutional supercooling begins when the actual liquid-temperature gradient at the interface is smaller than the liquidus gradient:
Using the solutions above, this is
At criticality the inequality is an equality. If , then and, for ,
The critical curve is proportional to . If , put to obtain
This curve behaves as for small and approaches for large . Supercooling occurs above the corresponding critical curve, where solute rejection steepens the liquidus faster than heat transport raises the actual temperature.

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