Structure of the Synthetic K-rich Phyllomanganate Birnessite Obtained by High-Temperature Decomposition of KMnO4. Substructures of K-rich Birnessite from 1000°C Experiment

Anne-Claire Gaillot (1) , Victor A. Drits (1, 2) , Alain Manceau (1) , Bruno Lanson (1)

1 LGIT - Laboratoire de Géophysique Interne et Tectonophysique
2 Geological Institute of the Russian Academy of Sciences

The structure of a synthetic potassium-rich birnessite prepared from the thermal decomposition of KMnO4 at 1000°C in air has been refined by Rietveld analysis of the powder X-ray diffraction (XRD) data, and the structure model shown to be consistent with extended X-ray absorption fine structure data. K-rich birnessite structure is a two-layer orthorhombic polytype (2O) with unit-cell parameters a = 5.1554(3) Ä, b = 2.8460(1) Ä, c = 14.088(1) Ä, α = β = γ = 90°, a/b = √3.281, and was refined in the Ccmm space group. The structure is characterized by the regular alternation of octahedral layers rotated with respect to each other by 180°. Octahedral layers are essentially devoid of vacant sites, the presence of 0.25 Mn 3+ layer cations within these layers being the main source of their deficit of charge, which is compensated for by interlayer K + cations. Mn3+ octahedra, which are distorted by the Jahn-Teller effect, are systematically elongated along the a axis (cooperative Jahn-Teller effect) to minimize steric strains, thus yielding an orthogonal layer symmetry. In addition, Mn 3+ octahedra are segregated in Mn3+-rich rows parallel to the b axis that alternate with two Mn 4+ rows according to the sequence ...-Mn3+-Mn4+-Mn4+-Mn3+-... along the a direction, thus leading to a A = 3a super-periodicity. At 350°C, the structure partially collapses due to the departure of interlayer H2O molecules and undergoes a reversible 2O-to-2H phase transition. This transition results from the relaxation of the cooperative Jahn-Teller effect, that is from the random orientation of elongated Mn 3+ octahedra.

Mots clés: Mn oxide; Birnessite; Phyllomanganate; XRD

Domaines: Minéralogie

Anne-Claire Gaillot, Victor A. Drits, Alain Manceau, Bruno Lanson. Structure of the Synthetic K-rich Phyllomanganate Birnessite Obtained by High-Temperature Decomposition of KMnO4. Substructures of K-rich Birnessite from 1000°C Experiment. Microporous and Mesoporous Materials, 2007, 98, pp.267-282. ⟨10.1016/j.micromeso.2006.09.010⟩. ⟨hal-00193628⟩