Pf. Romkens et al., INTERACTION BETWEEN CA2-CARBON - IMPLICATIONS FOR METAL MOBILIZATION(AND DISSOLVED ORGANIC), Applied geochemistry, 11(1-2), 1996, pp. 109-115
To investigate the role of dissolved Ca on the sorption and complexati
on behaviour of dissolved organic carbon (DOC), and the effect on diss
olved Cu concentration, batch sorption studies and titration experimen
ts have been performed. Both adsorption and desorption studies showed
that the DOC concentration depends on the presence of Ca. With increas
ing Ca content, the DOC concentration decreased as a result of sorptio
n and precipitation processes. The formation of aqueous Ca-DOC complex
es could be described well with a 1:1 Ca:DOC ratio. Log K-CaDOC values
for the formation of Ca-DOC complexes ranged from 3.7 to 4 in the low
pH range (3.5 to 6, interaction with carboxyl groups) and from 5.8 to
6 in the pH range from 7 to 9 (interaction with phenolic groups). The
results indicate that a large part of the available DOC is in a Ca fo
rm at near neutral pH values. In batch sorption experiments, the addit
ion of Ca2+ significantly reduced the DOC as well as the Cu concentrat
ion in solution. This indicates that sorption of Ca-DOC complexes at n
ear neutral pH is more important in regulating the Cu solution concent
ration compared to cation exchange processes. (C) 1996 Elsevier Scienc
e Ltd