Environmental Engineering Reference
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Total DOC
Hydrophilic DOC
Hydrophobic DOC
Metal concentration (mmol L -1 )
+
, Ca 2 +
, Al 3 +
and Fe 3 +
Fig. 8 Effects of increasing concentrations of Na
on the total, hydro-
philic and hydrophobic DOC at three pH levels (2.1, 4.0 and 6.5) and an initial total DOC con-
centration of 1.0 mmol L
1 . Data source Kaiser ( 1998 )
DOC-facilitated transport of elements (Reszat and Hendry 2007 ). The ability of
actinide ions such as uranyl to form complexes with DOC is very variable depend-
ing on the occurrence of humic fractions (fulvic and humic acids) in DOM, which
undergo in turn large variations (5-80 %) in the aquatic environments (Mostofa et
al. 2009a ; Kim and Czerwinski 1996 ; Giesy et al. 1986 ; Kim et al. 1994 ; Artinger
et al. 2002 ; Crancon and van der Lee 2003 ; Jackson et al. 2005 ). Interestingly, the
complexation of U to DOM is kinetically controlled (Artinger et al. 2002 ).
Studies on M-DOM complexation suggest that trace metals with high binding
strength are primarily distributed in the larger molecular size fractions, and met-
als with low binding strength are mostly distributed in the smaller molecular size
fractions (Wu et al. 2004b ; Shin et al. 2001 ; Lakshman et al. 1993 ; Midorikawa
and Tanoue 1996 , 1998 ; Lin et al. 1995 ; Rao and Choppin 1995 ; Sekaly et al.
1998 ; Sposito et al. 1982 ). The larger molecular size fractions have a higher affin-
ity for metals such as Al, Cu, UO 2 (II), and Np(V) than smaller molecular size
fractions (Shin et al. 2001 ; Lakshman et al. 1993 ; Midorikawa and Tanoue 1998 ;
Lin et al. 1995 ; Midorikawa and Tanoue 1996 ; Rao and Choppin 1995 ; Sekaly
et al. 1998 ; Sposito et al. 1982 ). Kinetic studies show that strong affinity metals
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