An experimental study of the solubility and speciation of niobium in fluoride-bearing aqueous solutions at elevated temperature

被引:143
|
作者
Timofeev, A. [1 ]
Migdisov, Art. A. [1 ]
Williams-Jones, A. E. [1 ]
机构
[1] McGill Univ, Dept Earth & Planetary Sci, Montreal, PQ H3A 0E8, Canada
基金
加拿大自然科学与工程研究理事会;
关键词
MOLAL THERMODYNAMIC PROPERTIES; RARE-EARTH-ELEMENTS; ACTIVITY-COEFFICIENTS; FLUID INCLUSION; STANDARD; DEPOSIT; PREDICTION; IONS;
D O I
10.1016/j.gca.2015.02.015
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 Nb2O5 and the speciation of niobium in HF-bearing aqueous solutions have been determined at temperatures of 150, 200, and 250 degrees C and saturated water pressure. At a pH of similar to 2 and at low HF concentration, niobium is transported primarily as the species Nb(OH)(4)(+) and at high HF concentration, as the species NbF2(OH)(3)degrees. Equilibrium constants for the formation of Nb(OH)(4)(+) range from -11.23 +/- 0.26 to -10.86 +/- 0.24 and for the formation of NbF2(OH)(3)degrees from -3.84 +/- 0.20 to -5.08 +/- 0.42, at 150 and 250 degrees C. The results of this study show that the solubility of Nb2O5 (solid) in aqueous fluids increases with increasing HF concentration, but is not strongly affected by temperature. The influence of pH is variable; at low pH and HF concentration, a decrease in pH increases the solubility of Nb2O5 (solid). At higher pH, the reverse may be true. Modeling of the transport and deposition of niobium suggests that simple mixing with a brine is not an effective method for removing niobium from solution. By contrast, interaction of an acidic fluid with carbonate rock results in a rapid reduction in the capacity of the fluid to mobilize niobium. (C) 2015 Elsevier Ltd. All rights
引用
收藏
页码:103 / 111
页数:9
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