Abstract
The iron bearing phases present in a ferromanganese nodule from the Central Indian Ocean have been determined using57Fe Mössbauer spectroscopy. The Mössbauer results have been corroborated by XRD, IR and TG-DTA studies. The Mössbauer spectrum of a ferromanganese nodule shows a broad line width which indicates the presence of more than one iron bearing paramagnetic oxide or oxyhydroxide phases where iron is present as Fe3+. γ-FeOOH has been distinctly characterised as one of the iron bearing phases in the nodule. Other oxyhydroxide and oxide phases of iron in the nodule have been ruled out. A typical paramagnetic doublet persists even at very high temperature which has been proposed to be due to iron(III)phosphate. Formation of solid solution of Mn2O3−Fe2O3 has been observed in the heat treated nodule at 1073 K, which has been characterised by the Mössbauer technique.
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Dutta, R.K., Das, D., Sudarshan, M. et al. 57Fe Mössbauer spectroscopic characterisation of a ferromanganese nodule from the Central Indian Ocean. J Radioanal Nucl Chem 223, 121–126 (1997). https://doi.org/10.1007/BF02223371
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DOI: https://doi.org/10.1007/BF02223371