A Reliable Method for Determining the Oxidation State of Manganese at the Microscale in Mn Oxides via Raman Spectroscopy

Manganese oxides are important geomaterials, widespread in terrestrial and Martian environments. Characterisation of the oxidation state of Mn is a central issue in science; this task has been addressed up to the present by X-ray spectroscopy or diffraction techniques. The former, however, requires access to synchrotron facilities, while the latter does not provide crystal-chemical information at the local scale. In this work, we compare a large set of Raman data from well-characterised samples, already published by the same authors of this paper or as found in the literature. We show a clear correlation between the oxidation state of Mn and the wavenumber of peculiar bands; octahedrally co-ordinated Mn2+ is recognised by a band around 530 cm(-1), Mn3+ by a band around 580 cm(-1) and Mn4+ by a band around 630 cm(-1), while tetrahedrally co-ordinated Mn2+ is recognisable by a band around 650 cm(-1). Strongly distorted Mn3+ octahedra are indicated by the appearance of Jahn-Teller modes. Our method allows a reliable, easily accessible tool to characterise the oxidation states of Mn in oxides, also suitable for microscale mapping. It provides a robust analytical basis for the use of these minerals as redox indicators in geology/geochemistry, in exoplanetary research or for monitoring technological processes.

Automated summary

The study characterizes the oxidation state of manganese using Raman spectroscopy data and establishes a clear correlation between the oxidation state of manganese ions and specific band wave numbers, providing a reliable analytical basis for using minerals as redox indicators and monitoring technological processes.