TY - JOUR
T1 - Deriving formation constants for aqueous metal complexes from XANES spectra
T2 - Zn2+ and Fe2+ chloride complexes in hypersaline solutions
AU - Liu, Weihua
AU - Etschmann, Barbara
AU - Foran, Garry
AU - Shelley, Michael
AU - Brugger, Joël
PY - 2007
Y1 - 2007
N2 - The development of numerical modeling of reactive transport relies on the availability of thermodynamic properties for the solid, surface, aqueous, and vapor species stable at the conditions of interest. The lack of experimental studies and comprehensive activity-composition models severely limits the predictive capabilities of these models in systems involving highly saline fluids or low-density volatile-rich fluids. X-ray absorption near-edge structure spectroscopy (XANES) is a powerful technique to study the speciation of transition metals in aqueous fluids: it is element specific; sensitive to the oxidation state of the metal, the ligand field and the coordination geometry of the complex; and it is suitable for measuring trace amounts of metals (<1 wt%) in solutions over a widepressure and temperature range. Formation constants for the aqueous complexes of transition metals can be determined from a series of XANES spectra obtained on solutions containing a constant amount of the metal of interest and variable concentrations of a ligand. The method relies on a non-linear, least-squares-fitting approach, with full distribution of species calculations based on a complete thermodynamic model for the experimental system under consideration. The technique is particularly suitable for following octahedral to tetrahedral transitions among weak chloride complexes of transition metals. The log K for the reaction Zn(octahedral)2+ + 4Cl- = ZnCl42+(tetrahedral) at 25 °C is retrieved to be 0.1(6), within error of the accepted literature value. The same method applied to Fe2+ -chloride complexes shows that the log K for the reaction Fe(octahedral)2+ + 4Cl- = FeCl42+(tetrahedral) increases from -6.2(6) at 25 °C to -2.9(3) at 150 °C. This study confirms that tetrahedral chloride complexes play an important role in Fe transport in hypersaline brines especially at elevated temperatures, and shows that XANES is well suited to study systems that may be difficult to study with other techniques.
AB - The development of numerical modeling of reactive transport relies on the availability of thermodynamic properties for the solid, surface, aqueous, and vapor species stable at the conditions of interest. The lack of experimental studies and comprehensive activity-composition models severely limits the predictive capabilities of these models in systems involving highly saline fluids or low-density volatile-rich fluids. X-ray absorption near-edge structure spectroscopy (XANES) is a powerful technique to study the speciation of transition metals in aqueous fluids: it is element specific; sensitive to the oxidation state of the metal, the ligand field and the coordination geometry of the complex; and it is suitable for measuring trace amounts of metals (<1 wt%) in solutions over a widepressure and temperature range. Formation constants for the aqueous complexes of transition metals can be determined from a series of XANES spectra obtained on solutions containing a constant amount of the metal of interest and variable concentrations of a ligand. The method relies on a non-linear, least-squares-fitting approach, with full distribution of species calculations based on a complete thermodynamic model for the experimental system under consideration. The technique is particularly suitable for following octahedral to tetrahedral transitions among weak chloride complexes of transition metals. The log K for the reaction Zn(octahedral)2+ + 4Cl- = ZnCl42+(tetrahedral) at 25 °C is retrieved to be 0.1(6), within error of the accepted literature value. The same method applied to Fe2+ -chloride complexes shows that the log K for the reaction Fe(octahedral)2+ + 4Cl- = FeCl42+(tetrahedral) increases from -6.2(6) at 25 °C to -2.9(3) at 150 °C. This study confirms that tetrahedral chloride complexes play an important role in Fe transport in hypersaline brines especially at elevated temperatures, and shows that XANES is well suited to study systems that may be difficult to study with other techniques.
KW - Fe and Zn chloride complexes
KW - Hydrothermal solutions
KW - Stability constants
KW - Thermodynamics
KW - XANES
KW - XAS
UR - http://www.scopus.com/inward/record.url?scp=34249785381&partnerID=8YFLogxK
U2 - 10.2138/am.2007.2225
DO - 10.2138/am.2007.2225
M3 - Article
SN - 0003-004X
VL - 92
SP - 761
EP - 770
JO - American Mineralogist
JF - American Mineralogist
IS - 5-6
ER -