Аннотация:
A simple method was proposed for calculating the composition of nonstoichiometric or partially oxidized magnetite, based on a linear relationship between the position of the (440) peak in the X-ray diffraction pattern and the completeness of material oxidation. The results obtained were verified by the Rietveld refinement method and showed the possibility of a principal assessment of the magnetite/maghemite ratio.
Образец цитирования:
L. S. Bondarenko, D. A. Pankratov, A. A. Dzeranov, G. I. Dzhardimalieva, A. N. Streltsova, M. Zarrelli, K. A. Kydralieva, “A simple method for quantification of nonstoichiometric magnetite nanoparticles using conventional X-ray diffraction technique”, Mendeleev Commun., 32:5 (2022), 642–644