Publication | Open Access
Structural incorporation of W<sup>6+</sup>into hematite and goethite: A combined study of natural and synthetic iron oxides developed from precursor ferrihydrite and the preservation of ancient fluid compositions in hematite
22
Citations
54
References
2016
Year
Rare Earth MineralEngineeringAncient Fluid CompositionsSolid-state ChemistryChemistryInorganic MaterialEnvironmental ChemistryMineral-fluid InteractionStructural IncorporationElemental CharacterizationW ContentMaterials ScienceInorganic ChemistrySynthetic Iron OxidesCrystallographyX-ray DiffractionGeochemistryPetrologyMineral Geochemistry
Hematite (a-Fe2O3) and goethite (a-FeOOH) can incorporate considerable amounts of tungsten (W). Although W concentrations up to several wt% in hematite and goethite have been reported in the literature, none of the proposed models for a structural incorporation has been generally accepted yet. Here, the first combination of X-ray absorption fine structure (XAFS) measurements with X-ray diffraction (XRD), Raman spectroscopy (RS), electron microprobe (EMPA) and total reflection X-ray fluorescence (TXRF) provides a general relation between W content and its structural incorporation into hematite and goethite.
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