Natural manganese oxide: Combined analytical approach for solid characterization and arsenic retention

To understand the retention of As on a natural manganese sand, the structural, textural and chemical properties of the solid were first investigated by combining scanning electron microscopy (SEM), transmission electron microscopy (TEM), electron-energy-loss spectroscopy (EELS), X-ray diffraction (X...

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Veröffentlicht in:Geochimica et cosmochimica acta 2005-06, Vol.69 (11), p.2715-2724
Hauptverfasser: Ouvrard, S., de Donato, Ph, Simonnot, M.O., Begin, S., Ghanbaja, J., Alnot, M., Duval, Y.B., Lhote, F., Barres, O., Sardin, M.
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Sprache:eng
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Zusammenfassung:To understand the retention of As on a natural manganese sand, the structural, textural and chemical properties of the solid were first investigated by combining scanning electron microscopy (SEM), transmission electron microscopy (TEM), electron-energy-loss spectroscopy (EELS), X-ray diffraction (XRD), BET N 2 gas adsorption, diffuse reflectance Fourier transform infrared (FT-IR) spectroscopy and X-ray photoelectron spectroscopy (XPS) analysis. Manganese sand could be mainly described as a mixture of a phyllomanganate, lithiophorite [(Al,Li)MnO 2(OH) 2], and pyrolusite (MnO 2). Iron particle, kaolinite and gibbsite type-phases were also observed. Particles organization led to the presence of a mesoporosity with pore diameters ranging from 100 to 200 Å and a specific surface area of 23 m 2 g −1. Contact with an As(V) solution (0.67 mmol L −1) led to an average fractional surface coverage of 0.4. Both As (V) and (III) were present on the surface of the sand in a 1:1 ratio. As(V) was sorbed on lithiophorite-type particles through surface complexation type reaction. As(III) was thought to result from As(V) reduction mechanism on iron particles.
ISSN:0016-7037
1872-9533
DOI:10.1016/j.gca.2004.12.023