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Article Dans Une Revue Journal of Geochemical Exploration Année : 2006

Structure of fougerite and green rusts and a thermodynamic model for their stabilities

Résumé

Fougerite is a new iron oxide, a mixed M(II)–M(III) hydroxide, a member of the green rust group. Its structure consists of a brucitic layer of Fe(III)–Fe(II)–Mg(II), where the excess of the positive charge due to Fe3+ is compensated in the interlayer by anions. The limits of composition are structurally and geochemically constrained, and the stabilities of the mineral and green rusts are obtained by a thermodynamic model of a regular solid solution, for different compensating anions and for any allowed composition of the brucitic layer

Domaines

Géochimie

Dates et versions

hal-02667649 , version 1 (31-05-2020)

Identifiants

Citer

Fabienne Trolard, Guilhem Bourrie. Structure of fougerite and green rusts and a thermodynamic model for their stabilities. Journal of Geochemical Exploration, 2006, 88 (1-3), pp.249-251. ⟨10.1016/j.gexplo.2005.08.048⟩. ⟨hal-02667649⟩

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