REVISED THERMODYNAMIC PROPERTIES OF BRUCITE DETERMINED BY SOLUBILITY STUDIES AND ITS SIGNIFICANCE TO NUCLEAR WASTE ISOLATION
There is a substantial discrepancy for DfGobrucite in recent publications, ranging from -830.4 (Harvie et al., 1984; Geochim. Cosmochim. Acta, 723751), through -831.9 (Brown et al., 1996; J. Chem. Soc., Dalton Trans., 30713075), through 833.5 (Robie and Hemingway, 1995; USGS Bull., 2131), and to 835.9 kJ mol1 (Konigsberger et al., 1999; Geochim. Cosmochim. Acta, 31053119). Using the DfGohydromagnesite (5424) from Konigsberger et al., the predicted log fCO2 for this assemblage would range from 5.96 (DfGobrucite from Harvie et al.) to 4.84 (DfGobrucite from Konigsberger et al.). Therefore, it is desirable to better constrain the DfGobrucite. For this reason, a series of solubility experiments involving brucite in NaCl solutions ranging from 0.01 M to 4.0 M have being conducted at SNL. The derived DfGobrucite from this study by extrapolation to infinite dilution via Pitzer formalism is 830.8 kJ mol1, which is in excellent agreement with recommended values of Harvie et al. and Brown et al.
ACKNOWLEDGEMENTS: This research is funded by WIPP programs administered by U.S. Department of Energy.
Sandia National Laboratories is a multiprogram laboratory operated by Sandia Corporation, a Lockheed Martin Company, for the United States Department of Energys National Nuclear Security Administration under Contract DE-AC04-94AL85000.