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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