Agriculture Reference
In-Depth Information
where ( S max ) 1 and ( S max ) 2 are the total number of type 1 sites and type 2 sites,
respectively. If F represents the fraction of type 1 sites to the total number of
sites or the adsorption capacity for an individual soil, we thus have:
(
)
=
F S
and(
)
=
(1
F S
)
S
S
max
(6.2)
max
max
max
1
2
We now denote ϕ as the number of unfilled or vacant sites in the soil, such that:
φ =
(
)
=
F SS
S
S
(6.3)
max
1
max
1
1
1
φ =
(
)
− =− −
(1
F SS
)
S
S
(6.4)
max
2
max
2
2
2
where ϕ and ϕ 2 are the number of vacant sites and S 1 and S 2 are the amounts
of solute retained (or the number of filled sites) on type 1 and type 2 sites,
respectively. As the sites become filled or occupied by the reactive solute, the
number of vacant sites approaches zero, that is, (ϕ 1 + ϕ 2 ) → 0. In the meantime,
the amount of solute retained by the soil matrix approaches that of the total
capacity (or maximum number) of sites, ( S 1 + S 2 ) → S max .
We commonly express the amount of reactive chemical retained, such as
S 1 and S 2 in Equations 6.3 and 6.4 as the mass of solute per unit mass of soil
(mg kg -1 soil). Based on the above formulations, the total number of sites S max ,
( S max ) 1 , and ( S max ) 2 and vacant or unfilled sites ϕ 1 and ϕ 2 must also have similar
dimensions. Here the units used for S and ϕ will be in terms of milligrams of
solute per kilogram soil mass (mg kg -1 soil).
Based on this approach, reactive chemical retention mechanisms are
assumed to follow a second-order kinetic reaction where the forward pro-
cess is controlled by the product of the solution concentration C (mg L -1 ) and
the number of unoccupied or unfilled sites (ϕ) (Selim and Amacher, 1988).
Specifically, the reactions for type 1 and type 2 sites may be expressed by the
reversible processes; t → ∞:
k
k
+ φ
C
1
S
(6.5)
1
1
2
and
k
k
+ φ
C
3
S
(6.6)
2
2
4
Therefore, the differential form of the kinetic rate equations for reactive
chemical retention may be expressed as:
ρ
S
t
1
=Θφ −ρ fortype1sites
C
k
k
S
(6.7)
1
2
1
1
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