longitudinal dispersion in nonuniform isotropic porous media
longitudinal dispersion in nonuniform isotropic porous media
longitudinal dispersion in nonuniform isotropic porous media
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185<br />
For a f<strong>in</strong>ite medium of length L, an appropriate boundary condition<br />
for the exit of the <strong>porous</strong> medium must be developed. Dankwerts (1953)<br />
aga<strong>in</strong> used a flux boundary condition<br />
- dCvc(L<br />
,t) - DL ax (L ,t) t > °<br />
where c e 1S the exit concentration, and L- refers to the exit <strong>in</strong>terface<br />
(x = L) as approached from x < L. Dankwerts (1953) argued, however,<br />
that c(L-,t) must equal c ,or the solute concentration with<strong>in</strong> the bed<br />
e<br />
would have to pass through a maximum or m<strong>in</strong>imum. The exit boundary<br />
condition is then,<br />
o t > ° (B.13)<br />
Brenner (1962) gives the solution to equation (B.5) with equations<br />
(B.8), (B.14) and the <strong>in</strong>itial condition<br />
to be<br />
C<br />
-=<br />
C o<br />
2exp [t (2X - T) ] x<br />
2/2<br />
X exp (-A k T 4P )<br />
c(x,O) = °<br />
° < x < L<br />
(B.14)