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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