The solubility of fluorite in Na-K-Cl solutions at temperatures up to 260 °C and ionic strengths up to 4 mol/kg H2O
- 1. Key Laboratory of High-temperature and High-pressure Study of the Earth's Interior, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002 (China)
- 2. Institute for Ecological Civilization of Karst Area, Guizhou Normal University, Guiyang 550001 (China)
- 3. Central European Institute of Technology, Brno University of Technology, Brno 61200 (Czech Republic)
- 4. Department of Geology and Pedology, Mendel University in Brno, Brno 61300 (Czech Republic)
- 5. University of Chinese Academy of Sciences, Beijing 100039 (China)
Description
The solubility of fluorite in hydrothermal conditions is important in ore forming and geothermal processes and groundwater utilization. However, a quantitative description of the geochemical behavior of fluorite under hydrothermal conditions has not been previously reported. In this work, the solubility of fluorite in Na-K-Cl solutions at temperatures up to 260 °C and ionic strengths up to 4 M was determined by experiments and modeling. The solubility products obtained in this work at 30 and 50 °C under ambient pressure and those from literature were used to regress the density model parameters for fluorite solubility product calculation at high temperature. The Pitzer interaction model was adopted to calculate the activity coefficient. The fluorite solubility determined in KCl solution at 250 °C under vapor saturated pressure and that from the literature were combined with the low-temperature thermodynamic properties of heat capacity and osmotic coefficient to obtain the binary parameters of NaF and KF at temperatures up to 260 °C. A thermodynamic model was then developed for calculating the fluorite solubility in Na-K-Cl solution at temperatures up to 260 °C, under vapor saturated pressure and ionic strengths up to 4 M. As calculated from this model, fluorite solubility measured at 200 °C and 0.1 M NaCl was well predicted. Both temperature and ionic strength had significant effects on fluorite solubility, and fluorite exhibited a similar dissolution pattern in both NaCl and KCl solution. When the concentration was lower than 2 M, the solubility of fluorite first increased with temperature, reached a maximum at approximately 100 °C, and then decreased. When the concentration was higher than 2 M, the solubility of fluorite increased monotonically with temperature. - Highlights: • The solubility product of fluorite can be calculated at temperatures up 260 °C. • The binary Pitzer parameters of NaF and KF at temperatures up to 260 °C were obtained. • Fluorite solubility can be calculated at temperatures up to 260 °C and ionic strengths up to 4 M in Na-K-Cl solution. • Fluorite dissolution behavior affected by both temperature and ionic strength and is similar in NaCl and KCl solution.
Availability note (English)
Available from http://dx.doi.org/10.1016/j.apgeochem.2017.04.017Additional details
Identifiers
- DOI
- 10.1016/j.apgeochem.2017.04.017;
- PII
- S0883-2927(16)30523-6;
Publishing Information
- Journal Title
- Applied Geochemistry
- Journal Volume
- 82
- Journal Page Range
- p. 79-88
- ISSN
- 0883-2927
- CODEN
- APPGEY
INIS
- Country of Publication
- United Kingdom
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 50071694
- Subject category
- S37: INORGANIC, ORGANIC, PHYSICAL AND ANALYTICAL CHEMISTRY; S58: GEOSCIENCES;
- Descriptors DEI
- FLUORITE; GEOCHEMISTRY; GROUND WATER; ORES; POTASSIUM CHLORIDES; POTASSIUM FLUORIDES; SODIUM CHLORIDES; SODIUM FLUORIDES; SOLUBILITY; SOLUTIONS; SPECIFIC HEAT; THERMODYNAMIC MODEL
- Descriptors DEC
- ALKALI METAL COMPOUNDS; CHEMISTRY; CHLORIDES; CHLORINE COMPOUNDS; DISPERSIONS; FLUORIDES; FLUORINE COMPOUNDS; HALIDE MINERALS; HALIDES; HALOGEN COMPOUNDS; HOMOGENEOUS MIXTURES; HYDROGEN COMPOUNDS; MATHEMATICAL MODELS; MINERALS; MIXTURES; OXYGEN COMPOUNDS; PARTICLE MODELS; PHYSICAL PROPERTIES; POTASSIUM COMPOUNDS; POTASSIUM HALIDES; SODIUM COMPOUNDS; SODIUM HALIDES; STATISTICAL MODELS; THERMODYNAMIC PROPERTIES; WATER
Optional Information
- Copyright
- Copyright (c) 2017 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.