Published April 2015
| Version v1
Journal article
Iron (III) sulfide particles produced by a polyol method
- 1. Tokyo University of Science (Japan)
- 2. The University of Electro-Communications (Japan)
Description
Iron(III) sulfide Fe2S3 particles were produced using a polyol method. Although pyrrhotite Fe1−xS appeared together with Fe2S3, the relative yield of Fe2S3 changed when the concentration of reagents in the oleylamine changed. Mössbauer spectra of the particles showed superparamagnetic doublets due to Fe2S3 at 293 K, along with a hyperfine magnetic splitting of H = 24.7 T at 6 K. XRD patterns of the Fe2S3 suggested a structure similar to that of greigite Fe3S4
Additional details
Identifiers
Publishing Information
- Journal Title
- Hyperfine Interactions
- Journal Volume
- 231
- Journal Issue
- 1-3
- Journal Page Range
- p. 115-121
- ISSN
- 0304-3843
- CODEN
- HYINDN
Conference
- Title
- 5. joint international conference on hyperfine interactions; International symposium on nuclear quadrupole interactions
- Acronym
- HFI/NQI 2014
- Dates
- 21-26 Sep 2014
- Place
- Canberra (Australia)
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 47037193
- Subject category
- S37: INORGANIC, ORGANIC, PHYSICAL AND ANALYTICAL CHEMISTRY;
- Resource subtype / Literary indicator
- Conference
- Descriptors DEI
- ABSORPTION SPECTRA; CONCENTRATION RATIO; CRYSTAL STRUCTURE; IRON; IRON SULFIDES; PARTICLES; PYRRHOTITE; SUPERPARAMAGNETISM; TEMPERATURE DEPENDENCE; X-RAY DIFFRACTION
- Descriptors DEC
- CHALCOGENIDES; COHERENT SCATTERING; DIFFRACTION; DIMENSIONLESS NUMBERS; ELEMENTS; IRON COMPOUNDS; MAGNETISM; METALS; MINERALS; SCATTERING; SPECTRA; SULFIDE MINERALS; SULFIDES; SULFUR COMPOUNDS; TRANSITION ELEMENT COMPOUNDS; TRANSITION ELEMENTS
Optional Information
- Copyright
- Copyright (c) 2015 Springer International Publishing Switzerland