Gallium speciation in aqueous solution. Experimental study and modelling .2. Solubility of alpha-GaOOH in acidic solutions from 150 to 250 degrees C and hydrolysis constants of gallium (III) to 300 degrees C

被引:71
作者
Benezeth, P
Diakonov, II
Pokrovski, GS
Dandurand, JL
Schott, J
Khodakovsky, IL
机构
[1] UNIV TOULOUSE 3,CNRS,LAB GEOCHIM,F-31400 TOULOUSE,FRANCE
[2] VI VERNADSKII INST GEOCHEM & ANALYT CHEM,MOSCOW 117334,RUSSIA
关键词
D O I
10.1016/S0016-7037(97)00012-4
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The solubility of alpha-GaOOH was measured in low ionic strength (0.025 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 to determine the dissociation constants (K-s0* to K-s3*) of the mineral from which hydrolysis constants of aqueous gallium species were derived. The dissociation constants generated in this study were used together with the thermodynamic properties of alpha-GaOOH (Pokrovski et al., 1997) to calculate the standard partial molal thermodynamic properties at 25 degrees C, 1 bar and the equations of state parameters for Ga3+, 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 calculation of gallium speciation as a function of pH and temperature. Our 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 increasing temperature, the amount of Ga(OH)(2)(+) and Ga(OH)(3)(0) becomes significant. These data are used to compare the geochemical behavior of Ga and Al in natural fluids. Copyright (C) 1997 Elsevier Science Ltd.
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页码:1345 / 1357
页数:13
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