Enthalpy method
243
with boundary conditions
c(>
=
-v,
H = 0
on
r =
a,
and initially
cf>=
-v,
H=O,
t=O,
outside s(r, t) = 0,
and
cf>
= 0,
H=M,
t=O,
within s(r, t) =
O.
The
conservative form of (6.69) across a surface of discontinuity s(r, t) =
0, obtained by integrating over a small volume,
is
[H]ds/dt=M
ds/dt =
[Vcf>
• Vs],
(6.70)
where [ ] denotes the jump between the sides where
H~O
and
H;;:.:M
respectively. Since
V2c(>
= 0 inside
the
anode
it
follows
that
(6.67)
is
satisfied by a solution of (6.69). Crowley (1979) obtained an implicit,
finite-difference solution for this problem by expressing (6.69) in cylindri-
cal polar coordinates.
Her
results are compared with those of Christian-
sen and Rasmussen (1976) and Elliott (1980) in Table 8.25.
The
flow of an incompressible fluid in a Hele-Shaw cell (Richardson
1972) (see §2.12.2) can be formulated in the same way (see Figs. 2.19,
20).
In
Crowley'S second problem the 'specific heat'
is
zero only in one
phase in which, therefore, an elliptic differential eqution holds, but we
have a parabolic equation in
the
other
phase. This is the situation for
saturated/unsaturated
flow
in a porous medium (Hornung 1978).
In
one
region the flow
is
unsaturated,
that
is
the medium is only partially filled
with fluid and its fluid content may change.
In
a second region the
medium is saturated and no more fluid can
be
added.
In
terms of a
velocity potential,
C(>,
the
relevant equation
is
(6.71)
where H measures
the
air content of
the
medium. Hornung (1978) adopts
the
'generalized-enthalpy relationships',
c(>
>0,
c(><0,
(6.72)
and
cf>
can
be
regarded as a generalized temperature. A sample problem
is
solved by Crowley (1979).
In
the
same paper, the uniqueness
of
the
weak solutions for these cases
in which
the
'specific heat' may vanish was proved by necessary exten-
sions
of
Oleinik's (1960) methods for the classical Stefan problem.
It
is
because zero specific heat means that temperature
is
no
longer a singie-
valued function of enthalpy
that
Oleinik's proof needs modification.
Crowley (1979) introduced a function strictly monotone in both
H and
C(>,
defined by
F(
cf>,
H)
= H +
'Ycf>
where
'Y
is
any positive constant, into the