
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