Quick Search:    advanced search

GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help

This Article Figures Only Full Text Full Text (PDF) Alert me when this article is cited Alert me if a correction is posted Citation Map Services Email this article to a friend Similar articles in this journal Similar articles in Web of Science Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via HighWire Citing Articles via Web of Science (5) Citing Articles via Google Scholar Google Scholar Articles by Allada, R. k. Articles by Sparks, D. L. Search for Related Content GeoRef GeoRef Citation

CALORIMETRIC DETERMINATION OF THE ENTHALPIES OF FORMATION OF HYDROTALCITE-LIKE SOLIDS AND THEIR USE IN THE GEOCHEMICAL MODELING OF METALS IN NATURAL WATERS

Rama kumar Allada^1,, Edward Peltier², Alexandra Navrotsky^1,*, William H. Casey³, C. Annette Johnson⁴, Hillary Thompson Berbeco⁵ and Donald L. Sparks²

¹ Thermochemistry Facility and NEAT ORU, Department of Chemical Engineering and Materials Science, University of California, Davis, CA 95616, USA
² Department of Plant and Soil Sciences, University of Delaware, Newark, DE 19716, USA
³ Department of Chemistry, University of California, Davis, CA 95616, USA
⁴ Swiss Federal Institute of Environmental Science and Technology (EAWAG), Postfach 611, CH-6800 Dübendorf, Switzerland
⁵ Franklin W. Olin College of Engineering, Needham, MA 02492, USA

^* E-mail address of corresponding author: anavrotsky{at}ucdavis.edu

Interest in hydrotalcite-like compounds has grown due to their role in controlling the mobility of aqueous metals in the environment as well as their use as catalysts, catalyst precursors and specialty chemicals. Although these materials have been studied in a number of contexts, little is known of their thermodynamic properties. High-temperature oxide melt solution calorimetry was used to measure the standard enthalpy of formation for compounds M(II)_1–xAl_x(OH)₂(CO₃)_x/2·mH₂O (0.2 < x < 0.4, M(II) = Mg, Co, Ni and Zn). The enthalpy of formation of these compounds from the relevant single cation phases was also determined. The formation of HTLCs results in a 5–20 kJ/mol enthalpy stabilization from the single cation hydroxides and carbonates and water. The data are correlated to two variables: the ratio of divalent to trivalent cation in the solid (M(II)/Al) and the identity of the divalent cation. It was observed that the M(II)/Al ratio exerts a minor influence on the enthalpy of formation from single-cation phases, while greater differences in stabilization resulted from changes in the chemical nature of the divalent cation. However, the data do not support any statistically significant correlation between the composition of HTLCs and their heats of formation. Equilibrium geochemical calculations based upon the thermodynamic data illustrate the effect of HTLCs on the speciation of metals in natural waters. These calculations show that, in many cases, HTLCs form even in waters that are undersaturated with respect to the individual divalent metal hydroxides and carbonates. Phase diagrams and stability diagrams involving Ni-bearing HTLCs and the single-cation components are presented. The Ni(II) concentration as a function of pH as well as the stability diagram for the equilibrium among minerals in the CaO-NiO-Al₂O₃-SiO₂-CO₂-H₂O system at 298 K are plotted.

Key Words: Aqueous Solubilities • Calorimetry • Enthalpy of Formation • Hydrotalcite-like Solids

This article has been cited by other articles:

				S. Tumiati, G. Godard, N. Masciocchi, S. Martin, and D. Monticelli Environmental factors controlling the precipitation of Cu-bearing hydrotalcite-like compounds from mine waters. The case of the "Eve verda" spring (Aosta Valley, Italy) European Journal of Mineralogy, February 1, 2008; 20(1): 73 - 94. [Abstract] [Full Text] [PDF]