The surface complexation model is used to describe sorption experiments of inorganic mercury(II) in the presence of an amorphous silica, Aerosil 200, or an iron (hydr)oxide, the goethite alpha-FeOOH (Bayferrox 910). In the simulations, one assumes the formation of a monodentate surface complex &tbond;S&bond;OHg(+) and of ternary surface complexes with OH(-) surface groups, &tbond;S&bond;OHgOH and &tbond;S&bond;OHgCl, when chlorides are present in solution. Participation of the complex &tbond;S&bond;OHgCl has been especially evidenced.
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