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the modification of an interface condition. This becomes evident, for instance, by the fact
that in the classical Stefan model, the temperature completely determines the phases,
that is, the liquid region can be characterized by the condition u > 0, whereas u < 0
characterizes the solid region, where u = 0 is the melting temperature. The inclusion of
surface tension will no longer allow to determine the phases merely by the sign of u.
The main reason for introducing the Gibbs-Thomson correction u = an stems from
the need to account for so-called supercooling, in which a fluid supports temperatures
below its freezing point, or superheating, the analogous phenomena for solids; or dendrite
formation, in which simple shapes evolve into complicated tree-like structures. The effect
of supercooling can be in the order of hundreds of degrees for certain materials and is
required for nucleation, namely the forming of a new phase in a set previously occupied
by the parental phase, see [10, Chapter 1] and [52]. However, (1) does not account for
nucleation effects and can only be applied in the presence of impurities or of some other
mechanism inducing nucleation. Supercooling is an equilibrium phenomenon and is not
merely a transient effect. A simple argument for appreciating these equilibrium effects as
a first-order correction to the continuum mechanics is given in [8, pp. 209-210]: Suppose
that u = 0 is the equilibrium temperature between a sohd and liquid separated by a
planar interface. Then a certain amount of energy is required for an atom at the surface
to overcome the binding energy of the crystal lattice and become part of the the liquid
with lower binding energy. The amount of energy required to produce this transition
depends on the number of nearest neighbors in the crystal structure and on the number
of nearest neighbors of an atom on the surface. If the interface between the solid and
liquid is curved, then an atom on the interface has fewer nearest neighbors and one expects
that it will require less energy to produce a phase transition. If one considers a solid with
constant mean curvature (an ice ball) in equilibrium with its melt, then one expects the
prevailing temperature to be lower, and the Gibbs-Thomson condition indeed predicts
that u = —o/R, where R is the radius of the ball. Hence, the fluid is supercooled even at
equilibrium.
A more detailed account of this argument, which is well-known to scientists in solid
state physics and material science, can be found in [10, 32]. A more satisfactory argu-
ment leading to the same conclusion (and further generalizations) may be obtained from
statistical mechanics see [9, 33, 44]. In [29, 30], a theoretical framework is developed
starting from general thermodynamical laws which are appropriate to a continuum and
which include interfacial contributions for both energy and entropy.
The Stefan problem has been studied in the mathematical literature for over a century,
see [49, 42] and [53, pp. 117-120] for a historic account, and has attracted the attention
of many prominent mathematicians.
The (classical) Stefan problem is known to admit unique global weak solutions, pro-
vided the given functions u'
0
and b' have the physically correct signs; see for instance
[25,
26, 34] and [37, pp. 496-503]. It is important to point out that the existence of weak
solutions is closely tied to the maximum principle, see for instance the proofs in [25]. If
the natural sign conditions for uj and b' are obstructed, then the Stefan problem becomes
ill-posed, see [16] for instance.