Thermochemistry of natural potassium sodium calcium leonhardite and its cation-exchanged forms

Irina Kiseleva, Alexandra Navrotsky, Igor A. Belitsky, Boris A. Fursenko

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70 Scopus citations

Abstract

Leonhardite, a partially dehydrated laumontite, and its alkali variety, primary leonhardite, have been studied by high-temperature calorimetry. The enthalpies of formation from oxides and elements at 298 K are -306.7 ± 7.1 and -14214.6 ± 11.2 kJ/mol, respectively, for leonhardite, Ca2Al4Si8O24·7H2O, and -521.2 ± 10.5 and -14253.7 ± 13.5 kJ/ mol, respectively, for primary leonhardite of composition Ca1.3Na0.6K0.8Al4Si 8O24·7H2O. The values for primary leonhardite are significantly more negative. New calorimetric data for sodium and potassium oxides were obtained on the basis of thermochemical cycles involving carbonates. The enthalpies of drop solution are -113.10 ± 0.83 kJ/mol for Na2O and -193.68 ± 1.10 kJ/mol for K2O, giving enthalpies of solution of -170.78 ± 0.90 kJ/mol for Na2O and -260.98 ± 1.20 kJ/mol for K2O. The effects of exchange cations (K,Na) on energetics and dehydration were studied using cation-exchanged samples. Alkali substitution decreases thermal stability (decomposition on heating in air) but increases thermodynamic stability with respect to the oxides and elements. Equilibrium relations between leonhardite and alkali-feldspar, calculated on the basis of these data, show that primary leonhardite can form only from geothermal solutions having rather high ratios of alkali ions to Ca.

Original languageEnglish (US)
Pages (from-to)668-675
Number of pages8
JournalAmerican Mineralogist
Volume81
Issue number5-6
DOIs
StatePublished - 1996
Externally publishedYes

ASJC Scopus subject areas

  • Geophysics
  • Geochemistry and Petrology

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