The distribution of organic pigments in marine manganese nodules from the Northwest Indian Ocean

Glasby, G. P.; Hodgson, G. W.

doi:10.1016/0016-7037(71)90130-x

Cited by 8 publications

(1 citation statement)

References 19 publications

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“…From direct observations of the topotactic transformation, Bodeï et al (2007) concluded that todorokite can form from a magnesium-rich vernadite precursor. However, such an observation is still lacking in ambient air conditions and thus questions the origin of tectomanganates found in surface soils (Taylor et al, 1964;Glasby & Hodgson, 1971;Ross et al, 1976;McKenzie, 1989). Such a structural evolution would also have a significant impact on the fate of trace elements as phyllomanganates can sorb cations both as outer-and inner-sphere complexes on both lateral and basal surfaces, whereas tectomanganates can sorb ions only as an outer-sphere complex and possess a much lower specific surface area than that of phyllomanganates.…”

Section: Introductionmentioning

confidence: 99%

Solid-state transformation of nanocrystalline phyllomanganate into tectomanganate: influence of initial layer and interlayer structure

Grangeon

Lanson

2014

Acta Crystallogr Sect B

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In surficial environments, the fate of many elements is influenced by their interactions with the phyllomanganate vernadite, a nano-sized and turbostratic variety of birnessite. To advance our understanding of the surface reactivity of vernadite as a function of pH, synthetic vernadite (δ-MnO2) was equilibrated at pH ranging from 3 to 10 and characterized structurally using chemical methods, thermogravimetry and modelling of powder X-ray diffraction (XRD) patterns. With decreasing pH, the number of vacant layer sites increases in the octahedral layers of δ-MnO2 (from 0.14 per layer octahedron at pH 10 to 0.17 at pH 3), whereas the number of layer Mn(3+) is, within errors, equal to 0.12 per layer octahedron over the whole pH range. Vacant layer sites are capped by interlayer Mn(3+) sorbed as triple corner-sharing surface complexes (TC sites). The increasing number of interlayer Mn(3+) with decreasing pH (from 0.075 per layer octahedron at pH 10 to 0.175 at pH 3) results in the decrease of the average Mn oxidation degree (from 3.80 ± 0.01 at pH 10 to 3.70 ± 0.01 at pH 3) and in the lowering of the Na/Mn ratio (from 27.66 ± 0.20 at pH 10 to 6.99 ± 0.16 at pH 3). In addition, in-plane unit-cell parameters are negatively correlated to the number of interlayer Mn at TC sites and decrease with decreasing pH (from b = 2.842 Å at pH 10 to b = 2.834 Å at pH 3), layer symmetry being systematically hexagonal with a = b × 3(1/2). Finally, modelling of X-ray diffraction (XRD) patterns indicates that crystallite size in the ab plane and along the c* axis decreases with decreasing pH, ranging respectively from 7 nm to 6 nm, and from 1.2 nm to 1.0 nm (pH 10 and 3, respectively). Following their characterization, dry samples were sealed in polystyrene vials, kept in the dark, and re-analysed 4 and 8 years later. With ageing time and despite the dry state, layer Mn(3+) extensively migrates to the interlayer most likely to minimize steric strains resulting from the Jahn-Teller distortion of Mn(3+) octahedra. When the number of interlayer Mn(3+) at TC sites resulting from this migration reaches the maximum value of ∼ 1/3 per layer octahedron, interlayer species from adjacent layers share their coordination sphere, resulting in cryptomelane-like tunnel structure fragments (with a 2 × 2 tunnel size) with a significantly improved layer stacking order.

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