Evolution of the Fe3+ Ion Local Environment During the Phase Transition ε-Fe2O3 → α-Fe2O3 › Research Explorer

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Evolution of the Fe³⁺ Ion Local Environment During the Phase Transition ε-Fe₂O₃ → α-Fe₂O₃

Research output: Contribution to journal › Article › peer-review

DOI

https://doi.org/10.1007/s10948-017-4307-y
Final published version

S. S. Yakushkin
D. A. Balaev
A. A. Dubrovskiy
S. V. Semenov
K. A. Shaikhutdinov
M. A. Kazakova
G. A. Bukhtiyarova
O. N. Martyanov
O. A. Bayukov

Original language	English
Pages (from-to)	1209-1217
Number of pages	9
Journal	Journal of Superconductivity and Novel Magnetism
Volume	31
Issue number	4
DOIs	https://doi.org/10.1007/s10948-017-4307-y
Publication status	Published - 1 Apr 2018

Research areas

Magnetic properties, Mossbauer spectroscopy, Phase transition, Structure size effect, ε−FeO iron oxide nanoparticles, TRANSFORMATION, SILICA-GEL, FE2O3/SIO2, PARTICLES, NANOCRYSTALS, IRON, COERCIVE FIELD, GAMMA-FE2O3, NANOPARTICLES, epsilon-Fe2O3 iron oxide nanoparticles, MAGNETIC-PROPERTIES

OECD FOS+WOS

ID: 9916459