Spectral and chemical studies of iron and manganese oxyhydroxides in laterite developed on ultramafic rocks

Iron (Fe) oxyhydroxides (goethite and hematite) and manganese (Mn)‐oxyhydroxides (lithiophorite, asbolane, lithiophorite‐asbolane intermediate) are typically fine‐grained and poorly crystalline in nature, and as such are difficult to identify by conventional X‐ray powder diffraction. This study empl...

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Bibliographic Details
Published in:Resource geology 2021-10, Vol.71 (4), p.377-391
Main Authors: Tupaz, Carmela Alen J., Watanabe, Yasushi, Sanematsu, Kenzo, Echigo, Takuya
Format: Article
Language:English
Subjects:
Aluminum
Analytical methods
Chromium
Cobalt
Electron probe
Electron probe microanalysis
Fe‐ and Mn‐ oxyhydroxides
Goethite
Haematite
Hematite
Intermediates
Iron
Laterites
Manganese
Manganese oxyhydroxides
Minerals
Nickel
Ni–Co laterite deposit
Raman spectroscopy
Silicon
Spectroscopy
Spectrum analysis
Ultramafic materials
Ultramafic rocks
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Summary:Iron (Fe) oxyhydroxides (goethite and hematite) and manganese (Mn)‐oxyhydroxides (lithiophorite, asbolane, lithiophorite‐asbolane intermediate) are typically fine‐grained and poorly crystalline in nature, and as such are difficult to identify by conventional X‐ray powder diffraction. This study employs Raman spectroscopy and electron probe microanalysis (EPMA) to characterize Fe‐ and Mn‐oxyhydroxides found in the Berong Ni–Co laterite deposit at Palawan Island, Philippines. Accurate identification of these minerals is important because these phases contain high Ni and Co contents. Goethite and hematite occur in a wide range of textures, which are related to their compositional variations with respect to Ni, Al, Mn, Cr, and Si. The change in the intensity of the Raman peaks can be linked to the variable concentrations of Ni, Al, Mn, Cr, and Si in goethite. These chemical variations affect the textural transformation of goethite from amorphous to cryptocrystalline. Lithiophorite, asbolane and their intermediates were properly distinguished using Raman spectroscopy. EPMA data shows that these Mn minerals contain appreciable concentrations of Ni, Co, Al, and Fe. The band shift from lithiophorite to asbolane end terms in the 486–593 cm−1 domain indicates the substitution of Al in lithiophorite by Ni, Co, and Fe. Lithiophorite, lithiophorite‐asbolane intermediate, and asbolane were properly distinguished using Raman spectroscopy. Raman spectral changes within Mn minerals indicate substitution of Al by Ni, Co, and Fe. The change in the intensity of the Raman peaks of goethite can be linked to the variable concentrations of Ni, Al, Mn, Cr, and Si.
ISSN:1344-1698
1751-3928
DOI:10.1111/rge.12272