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Fig. 13.5
Proposed model for abiotic reduction in a sorbing sediment system (Wolfe 1989 )
CH 3
O
H
H 3 C
S
C
H
N
O
C
N
CH 3
CH 3
Oxidation
Aldicarb
Reduction
CH 3
O
O
CH 3
O
H
H 3 CS C
H 3 C
S
H
N
O
C
N
H
CH 3
CH 3
CH 3
2-methyl-2methyl thiopropionaldehyde
Aldicarb sulfoxide
+
Oxidation
CH 3
H 3 C
S
C
N
O
CH 3
O
H
CH 3
H 3 C
S
H
N
O
C
N
CH 3
2-methyl-2methyl thiopropionitrile
O
CH 3
Aldicarb sulfone
Fig. 13.6
Redox transformation pathways of aldicarb (Macalady et al. 1986 ; Wolfe et al. 1986 )
retention, volatilization, dissolution, photolysis and surface-, chemically, and
biologically induced degradation can affect hydrocarbons in groundwater. Bio-
degradation is a major transformation process of petroleum hydrocarbons.
Both aerobic and anaerobic biological degradation control the persistence of
hydrocarbons in groundwater, such as the n-alkane group. A generalized biodeg-
radation pathway is presented in Fig. 13.7 . The aerobic pathway shows conversion
of an alkane chain to fatty acids, fatty alcohols, and aldehyde and carboxylic acids,
which are then channeled into the central metabolism for subsequent b-oxidation.
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