1.6.2 Freezing of a square solid: the two-dimensional Stefan problem

Products: ABAQUS/Standard  ABAQUS/Explicit  

Heat conduction problems involving latent heat effects occur often in practice (examples are metal casting and permafrost meltout) but are not simple to solve. In some cases the phase change occurs with little latent heat effect and rapid temperature changes can partially suppress the change, as in the case of the amorphous/crystalline polymer phase change. For such cases ABAQUS/Standard provides a user subroutine, HETVAL, in which the user can program the kinetics of the phase change and the consequent latent heat exchange in terms of solution-dependent state variables. In contrast, a liquid/solid phase change is usually fairly abrupt and is accompanied by a strong latent heat effect. This case is the one considered in this example.

The problem is the two-dimensional Stefan problem (Figure 1.6.2–1): a square block of material is initially liquid, just above the freezing temperature. The temperature of its outside perimeter is reduced suddenly by a large value, so that the block starts to freeze from the outside toward the core. The freezing has a very large latent heat effect associated with it that dominates the solution. The problem has no exact solution, but a number of researchers have provided approximate solutions. Probably the most accurate of these is the numerical solution of Lazaridis (1970), who considers the problem as a moving boundary condition problem. Lazaridis's solution is used here as verification of the ABAQUS modeling of such cases.

Problem description

Material

The material properties (in consistent units) are

Density1.0
Specific heat1.0
Latent heat of freezing70.26
Freezing temperature
Thermal conductivity1.08

This set of values includes a latent heat effect that is far more severe than that in any material of practical importance. This value is deliberately chosen to provide a stringent test of the accuracy of the algorithm.

The latent heat must be specified in ABAQUS over a temperature range. For this purpose we give the solidus and liquidus temperatures as –0.25° and –0.15°, respectively.

In the simulations involving ABAQUS/Explicit dummy mechanical properties are used to complete the material definition.

Boundary conditions

The symmetry lines are insulated; this is the default surface boundary condition and, so, need not be specified. The outside surfaces must be reduced at time zero to –45°. This value can be specified directly; however, we ramp the temperature down to –45° over a time of 0.05 to prevent the automatic time incrementation scheme in ABAQUS/Standard from choosing very small time increments at the beginning of the simulation.

Time increment controls

Automatic time incrementation is chosen, which is the usual option for transient heat conduction problems. In ABAQUS/Standard a maximum temperature change of 4° is allowed per time increment to allow the time increment to increase to large values at later times as the solution smoothes out.

Results and discussion

Input files

Reference

Figures

Figure 1.6.2–1 Square plate freezing example.

Figure 1.6.2–2 Square plate fusion—temperature versus time at nodes A and B of Figure 1.6.2–1 (ABAQUS/Standard).

Figure 1.6.2–3 Square plate fusion—isotherms at 0.450 (ABAQUS/Standard).

Figure 1.6.2–4 Square plate fusion—isotherms at 5.0 (ABAQUS/Standard).

Figure 1.6.2–5 Comparison of results obtained with ABAQUS/Explicit and ABAQUS/Standard.