Russian Journal of Inorganic Chemistry · 2006 · 19 citations · 12 references
Natural SciencesChemistryEarth SciencesInorganic ChemistryMineralogySpectroscopyIron OxidesMineral ChemistryMineral GeochemistryOxide MineralsRedox ProcessesX-ray Photoelectron SpectroscopyFerromanganese OxidesHematiteIron Redox Chemistry
The sorption behavior is studied and the physicochemical neptunium species existing on the surface of goethite (α-FeOOH), maghemite (γ-Fe2O3), and hematite (α-Fe2O3) are determined. Solvent extraction and X-ray photoelectron spectroscopy (XPS) are used to determine the neptunium surface species. The ion and elemental composition of the surface of the minerals and surface neptunyl NpO 2 + complexes is determined using these data. Compounds containing neptunium(IV) or neptunium(VI) ions do not appear; rather, neptunyl (Np(V)O 2 + group is complexed with surface hydroxide groups of α-FeOOH, γ-Fe2O3, and α-Fe2O3. Presumably, the oxygen atoms of iron oxides and water and/or carbonate (CO 3 2- ) or nitrate (NO 3 - ) group lie in the equatorial plane of the neptunyl (NpO 2 + ) group.
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THE ZERO POINT OF CHARGE OF OXIDES<sup>1</sup>
G.A. Parks, P.L. De Bruyn · The Journal of Physical Chemistry · 1962 · 802 citations