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European Journal of Mineralogy; January, February 2004; v. 16; no. 1; p. 85-90; DOI: 10.1127/0935-1221/2004/0016-0085
© 2004 E. Schweizerbart'sche Verlagsbuchhandlung Science Publishers
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Articles

Hydrothermal synthesis of aegirine at 200°C

Alain DECARREAU*, Sabine PETIT, Philippe VIEILLARD and Nathalie DABERT

UMR CNRS 6532 HYDRASA, Université de Poitiers, 40 avenue du Recteur Pineau, F-86022 Poitiers Cedex, France

* E-mail: alain.decarreau{at}hydrasa.univ-poitiers.fr

Aegirine is synthesized at temperatures as low as 200°C in the system Si, Fe, Na, H2O. Aegirine is mixed with a poorly crystallized 2:1 ferric phyllosilicate. At lower temperature, only 2:1 phyllosilicates are synthesized. A thermodynamic approach shows that the synthesized aegirine is in equilibrium with ferripyrophyllite, and that the stability field of aegirine at lower temperature is strongly reduced by a 2:1 phyllosilicate with a tetrahedral charge due to tetrahedral substitutions of Si for Fe3+.

Key-words: aegirine, synthesis, low-temperature, thermodynamic.




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