Comment on “Integrated Mineralogical Characterization of Banded Iron Ores of Orissa and Its Implications on Beneficiation” by Mohanty et al. (2012), Journal of Minerals and Materials Characterization and Engineering, 11, 1133-1142*
Mohanty et al. (2012) have wrongly analyzed M?ssbauer spectra obtained from various iron ore samples. We criticized their approach suggesting suitable methodology, and suggested to refer earlier work carried out by Nayak et al. (2001, 2004) on representative samples from the same geological belt.
References
[1]
J. K. Mohanty, M. S. Jena and A. K. Paul, “Integrated Mineralogical Characterisation of Banded Iron Ores of Orissa and Its Implications on Beneficiation,” Journal of Minerals and Materials Characterization and Engineering, Vol. 11, No. 12, 2012, pp. 1133-1142.
[2]
P. K. Nayak, D. Das, V. Vijayan, P. Singh and V. Chakravorty, “57Fe M?ssbauer and EDXRF Studies on Three Representative Banded Iron Formations (BIFs) of Orissa, India,” Nuclear Instruments and Methods in Physics Research Section B, Vol. 184, No. 4, 2001, pp. 649-654.
[3]
P. K. Nayak, D. Das, P. Singh and V. Chakravorty, “57Fe M?ssbauer Spectroscopy of Banded Iron Formations from Eastern India,” Journal of Radioanalytical and Nuclear Chemistry, Vol. 260, No. 1, 2004, pp. 19-26.
[4]
P. K. Nayak et al., “Quantitative multielemental analysis of Titaniferous Magnetites by PIXE, EDXRF, and Their Iron Mineral Characterization by 57Fe M?ssbauer Spectroscopy,” Journal of Radioanalytical and Nuclear Chemistry, Vol. 254, No. 2, 2002, pp. 351-356.
