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Collection and Analysis of High Temperature-Resolution 57Fe Mössbauer Spectroscopy for Detailed Iron Mineral Characterisation.

Created on 24 Sep 2026

Authors

Andrew R C Grigg, James M Byrne, Ruben Kretzschmar

Published in

Chemphyschem : a European journal of chemical physics and physical chemistry. Volume 27. Issue 18. Pages e70557. Sep 28, 2026.

Abstract

57Fe Mössbauer spectroscopy is a powerful technique for determining the oxidation state and magnetic properties of Fe-bearing materials. Since magnetic properties are temperature dependent, Mössbauer spectra are often collected at multiple temperatures, especially around characteristic transition points such as the magnetic blocking temperature. Mössbauer data acquisition times are slow, sometimes taking >24 h to achieve high signal-to-noise ratios (SNR), which limits the number of spectra that can be collected. Here we propose an alternative approach, measuring profiles with high temperature resolution (e.g. 1 K temperature steps) but lower SNR. Using ferrihydrite with varying crystallinity as examples, we revealed mineralogical properties with increased detail even without large increases in the total acquisition time. The temperature dependence of the hyperfine parameters was clearly revealed in qualitative analysis, while simultaneous quantitative analysis of the spectra in both the temperature and energy domains revealed details about the distribution of particle crystallinity in pure ferrihydrite and mixed-phase samples. This approach will improve the measurement of temperature-dependent mineral properties, enabling analysis of blocking temperature distributions, improving the interpolation of hyperfine parameters in temperature profiles and aiding the discrimination of overlapping spectra in mixed-phase samples.

PMID:
42778503
Bibliographic data and abstract were imported from PubMed on 24 Sep 2026.

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