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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)

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