Abstract
The thermodynamic stability constants for the hydrolysis and formation of mercury (Hg2+) chloride complexes
$$ \hbox{Hg}^{2+} + n\hbox{H}_{2}\hbox{O} = \hbox{Hg(OH)}_n^{(2-n)+} + n\hbox{H}^{+ } \quad\quad \beta_n $$
$$ \hbox{Hg}^{2+} + n\hbox{Cl}^{-} = \hbox{HgCl}_n^{(2-n)+ } \quad\quad \beta_i $$
have been used to calculate the activity coefficients for Hg(OH)
n
(2–n)+
and HgCl
n
(2–n)+
complexes using the Pitzer specific interaction model. These values have been used to determine the Pitzer parameters for the hydroxide and chloro complexes
$$(\beta_{\rm ML}^{(0)}, \,\beta_{\rm ML}^{(1)}$$
and C
ML). The values of
$$\lambda_{ij}$$
and
$$\zeta_{ijk}$$
have been determined for the neutral complexes (Hg(OH)2 and HgCl2). The resultant parameters yield calculated values for the measured values of log
$$\beta^{\ast}$$
to ±0.01 from I = 0.1 to 3 m at 25°C. Since the activity coefficients of
$$\hbox{Hg(OH)}_n^{(2-n)+}$$
and
$$\hbox{HgCl}_n^{(2-n)+}$$
are in reasonable agreement with the values for Pb(II), we have estimated the effect of temperature on the chloride constants for Hg(II) from 0 to 300°C and I = 0–6 m using the Pitzer parameters for
$$\hbox{PbCl}_n^{(2-n)+}$$
complexes. The resulting parameters can be used to examine the speciation of Hg(II) with Cl− in natural waters over a wide range of conditions.
