F. Trolard et al., EVIDENCE OF THE OCCURRENCE OF A GREEN RUS TS COMPONENT IN HYDROMORPHIC SOILS - PROPOSITION OF THE EXISTENCE OF A NEW MINERAL - FOUGERITE, Comptes rendus de l'Academie des sciences. Serie II. Sciences de la terre et des planetes, 323(12), 1996, pp. 1015-1022
The natural occurrence of green rusts in soils is demonstrated for the
first time on the basis of the simultaneous study of the reactivity a
nd the structure of these compounds. A mixed Fe(II)-Fe(III) oxide tran
sforms by oxidation into lepidocrocite and goethite, readily dissolves
in the citrate-bicarbonate reagent without the necessity of a previou
s reduction, and shows Mossbauer and Raman spectra that enable us to i
dentify it unambiguously as a green rust, by comparison with synthetic
minerals.