Agriculture Reference
In-Depth Information
three exact solutions to the CDE (Equation 3.24) that are widely cited in the
literature. All three solutions have the form:
+−
(
)
Az t
(,)
0
<<
t
CCC
t
i
o
i
p
Czt
(,)
=
(3.48)
+− −
(
)
Azt
(,)
C Az t
(
,
)
t
>
CCC
t
t
i
o
i
o
p
p
where we assume a simple initial condition ( C = C i ) representing uniform
solute concentration distribution in the soil at t = 0. The form of the solution
in Equation 3.33 is applicable for conditions representing continuous solute
application or a pulse-type input having duration t p . For the three exact solu-
tions, the appropriate expressions for A ( z , t ) are given below.
3.5 Brenner Solution
Brenner (1962) considered the case of a finite soil column with the more pre-
cise third-type boundary condition at z = 0 that accounts for dispersion and
advection across the upper surface (Equations 3.29 and 3.30). By defining the
Peclet number defined in Equation 3.31
P= vL
D
(3.50)
Brenner's solution can be expressed as:
2
ββ β
z
+
P
β
z
zP
L
Pvt
LR
β
vt
PLR
2
P
cos
m
sin
m
exp
m
mm
L
2
L
24
Azt
(,)1
=−
2
2
P
P
2
2
β ++
P
β +
m
=
1
m
m
4
4
(3. 51)
where the eigenvalues β m are the positive roots of
2
β − β
P
4
m
β
cot
() P
+
=0
(3.52)
m
m
Brenner's solution describes volume-averaged concentrations within the
column. Because of the zero concentration gradient at z = L , this solution also
defines a flux concentration at the lower boundary. Hence, Brenner's solution
correctly interprets effluent concentrations as representing flux-averaged
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