GALLIUM SPECIATION IN AQUEOUS-SOLUTION - EXPERIMENTAL-STUDY AND MODELING .2. SOLUBILITY OF ALPHA-GAOOH IN ACIDIC SOLUTIONS FROM 150-DEGREES-C TO 250-DEGREES-C AND HYDROLYSIS CONSTANTS OF GALLIUM(III) TO 300-DEGREES-C
P. Benezeth et al., GALLIUM SPECIATION IN AQUEOUS-SOLUTION - EXPERIMENTAL-STUDY AND MODELING .2. SOLUBILITY OF ALPHA-GAOOH IN ACIDIC SOLUTIONS FROM 150-DEGREES-C TO 250-DEGREES-C AND HYDROLYSIS CONSTANTS OF GALLIUM(III) TO 300-DEGREES-C, Geochimica et cosmochimica acta, 61(7), 1997, pp. 1345-1357
The solubility of alpha-GaOOH was measured in low ionic strength (0.02
5 M) HCl-NaCl solutions over the pH range 1.6-4.1 at 150, 200, and 250
degrees C. A least squares linear regression of these data was used t
o determine the dissociation constants (K-s0 to K-s3*) of the mineral
from which hydrolysis constants of aqueous gallium species were deriv
ed. The dissociation constants generated in this study were used toget
her with the thermodynamic properties of alpha-GaOOH (Pokrovski et al.
, 1997) to calculate the standard partial molal thermodynamic properti
es at 25 degrees C, 1 bar and the equations of state parameters for Ga
3+, Ga(OH)(2+), Ga(OH)(2)(+), and Ga(OH)(3)(0) within the framework of
the revised HKF model (Tanger and Helgeson, 1988; Shock and Helgeson,
1988; Shock et al., 1992). These thermodynamic properties enabled cal
culation of gallium speciation as a function of pH and temperature. Ou
r results indicate that the hydrolysis of Ga occurs at low pH and its
speciation is strongly dominated by the negatively-charged species Ga(
OH)(4)(-) in the pH range of natural solutions at 25 degrees C. At inc
reasing temperature, the amount of Ga(OH)(2)(+) and Ga(OH)(3)(0) becom
es significant. These data are used to compare the geochemical behavio
r of Ga and Al in natural fluids. Copyright (C) 1997 Elsevier Science
Ltd.