磁铁矿纳米粉体的超细相互作用与磁性能

S. Yuryev, S. Yushchuk, F. Tsiupko, S. Dubelt, V. Loboiko
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引用次数: 0

摘要

用浓NH4OH沉淀化学纯摩尔盐Fe(NH4)2(SO4)2·6H2O和FeCl3的水溶液,得到磁铁矿Fe3O4的细粉。得到了粒径为5 ~ 25nm的细粉。部分粉末在473,573和673 K的空气中进行热处理。这种退火导致了γ-Fe2O3的形成。用核磁共振法(NGR)获得了这些离子在Fe3O4和γ-Fe2O3晶体结构中的超精细相互作用参数,并揭示了铁离子在八晶格和四晶格中的占据与化学计量磁铁矿的不同。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Hyperfine interactions and magnetic properties of nanosized powders of magnetite
The fine powder of magnetite Fe3O4 was obtained by precipitation of aqueous solutions of chemically pure Mohr's salt Fe(NH4)2(SO4)2·6H2O and FeCl3 using concentrated NH4OH. The fine powders with the particle size from 5 to 25 nm were obtained. Some portions of powders were subjected to heat treatment in air at temperatures of 473, 573 and 673 K. This annealing leads to the formation of γ-Fe2O3. The parameters of hyperfine interactions for these ions in the crystal structure of Fe3O4 and γ-Fe2O3 by the nuclear gamma-resonance method (NGR) were obtained and difference in occupations of iron ions in octa- and tetra-sublattice compared to stoichiometric magnetite was revealed.
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