Environmental Engineering Reference
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2.6 Kinetics of Photoinduced Degradation of DOM
Photoinduced degradation can decrease the concentration of dissolved organic car-
bon (DOC) as a function of the integrated solar intensity (Fig. 7 ) (Mostofa et al.
2005 , 2007 ). The changes in the DOC concentration can be best fit with a first
order reaction as reported below (Eq. 2.47 ):
Ln ( DOC / DOC o ) =− k 1 S
(2.47)
where k 1 is the reaction rate constant for the photoinduced degradation of DOC,
DOC is organic carbon concentration after irradiation and DOC o the initial
one, and S is the integrated solar intensity or photon energy (MJ m 2 ) (Fig. 7 a)
(Mostofa et al. 2007 ).
Kinetics studies on the photoinduced degradation of DOM can explain several
important phenomena in waters (Mostofa et al. 2007 ). First, stream DOM under-
goes rapid photoinduced degradation (1.8-2.6 × 10 3 MJ 1 m 2 in waters of the
Kago and Nishi-Mataya upstreams) (Mostofa et al. 2007 ). Second, microbial
degradation under dark incubation is quite low or negligible for upstream DOM
(0.7-4.6 × 10 4 MJ 1 m 2 for the same upstreams). Third, in rivers that include
various sources of DOM the latter can be uniformly degraded both photolytically
(9.5 × 10 4 MJ 1 m 2 ) and microbiologically (11 × 10 4 MJ 1 m 2 ) (Fig. 1 c and d).
3 Factors Controlling the Photoinduced Degradation
of DOM in Natural Waters
Photoinduced degradation of DOM depends on the sources of waters, concentra-
tion level and optical-chemical nature of DOM, time and space. Photoinduced
degradation of DOM is an important phenomenon that plays a significant role
in the biogeochemistry of the carbon cycle, biological activity and primary and
secondary productions in natural waters (Mostofa et al. 2009a ; Ma and Green
(a)
(b)
(c)
Integrated solar intensity (MJm
-2 )
2 ) in
the Kago upstream ( a ), Nishi-Mataya upstream ( b ), and in the downstream waters of Yasu River
( c ). Data source Mostofa et al. ( 2007 )
Fig. 7 Relationship between the Ln ( DOC / DOC 0 ) and the integrated solar intensity (MJm
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