Geoscience Reference
In-Depth Information
The kinetic equation for indirect photolysis is
dC / dt
=
- k 2 CX
=
- k p C
(4.85)
where
k 2
=
indirect photolysis rate constant
X
=
concentration of the nontarget intermediary
k p
=
overall pseudo-first-order rate constant for sensitized photolysis
4.2.4.7
Biodegradation
If the microbial community has adapted to the contaminant, the Michaelis-Menten
equation can be used to represent the rate of biotransformation as
k b
=
(
µ max X )/( Y ( k s
+
c ))
(4.86)
where
c
=
concentration of chemical being biodegraded [
µ
g m −3 ]
µ max
=
maximum growth rate of the culture [yr −1 ]
X
=
biomass concentration of the microorganisms [cells.m −3 ]
Y
=
yield coefficient [cells produced per mass toxicant removed]
k s
=
half-saturation constant [
µ
g.m −3 ]
k b
=
biological transformation rate constant [m 3 cells −1 year −1 ]
When c << k s , then
k b
=
(
µ max X )/( Y
k s )
=
k b 2
X
(4.87)
where k b 2 is the second-order biotransformation rate constant [m 3 cells −1 year −1 ].
For systems where the microbial population is relatively constant, the transfor-
mation rate equation reduces to a pseudo-first-order rate expression. 45
If pseudo-first-order rates are unavailable, or if they must be extrapolated to
different bacterial conditions, then the second-order approach can be used. It is
generally assumed that bacterial populations are unaffected by the presence of the
pollutant compound at low concentrations. Second-order kinetics for dissolved,
DOC-sorbed, and sediment-sorbed chemical can also be considered:
K BW
=
P ac ( t )
Σ i
Σ j k bij f ij
j
=
1, 2
(4.88)
K BS
=
P ac ( t )
Σ i
Σ j k bij f ij
j
=
3
(4.89)
where
K BW
=
total biodegradation rate constant in the water column [day −1 ]
K BS
=
total biodegradation rate constant on sediment [day −1 ]
k bij
=
second-order biodegradation rate constant for species i , phase j [ml cell −1 day −1 ]
P ac (t )
=
active bacterial population density in segment [cell ml −1 ]
f ij
=
fraction of chemical as species i in phase j
 
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