H. Hintelmann et al., MEASUREMENT OF COMPLEXATION OF METHYLMERCURY(II) COMPOUNDS BY FRESH-WATER HUMIC SUBSTANCES USING EQUILIBRIUM DIALYSIS, Environmental science & technology, 31(2), 1997, pp. 489-495
Humic and fulvic acids from lakes in Ontario, Canada, have been isolat
ed and been examined for their ability to bind methylmercury(II). Equi
librium dialysis has been applied to differentiate between bound and u
nbound fractions of MeHg(II). Losses of methylmercury(II) from solutio
ns containing 0.5-100 ng/L MeHg(II) and 10 mg/L humic substances (HS)
are negligible over a 24-h time interval when using acid cleaned glass
beakers, membrane closures, and cellulose ester membranes having a mo
lecular weight cutoff of 500. Dialysis equilibrium for MeHg(II) is rea
ched within this period of time. For each humic material, two classes
of binding sites could be detected. Log K values of conditional stabil
ity constants for the strong and the weaker binding sites were in the
range of 13.02-14.48 and 12.15-13.07, respectively. Binding capacities
have been calculated as 0.2-13 of ng MeHg(II)/mg of HS for the strong
sites and 1.2-72 ng of MeHg(II)/mg of HS for the weaker sites. Calcul
ation of equilibrium distribution shows that methylmercury(II)-HS comp
lexes predominate in oxidized freshwaters with low sulfide concentrati
ons. In anoxic waters, CH3HgSH should prevail. The CH3HgCl complex is
tao weak to compete with either of the latter complexes.