Oxidation of silicon from an Fe–6 at% Si alloy
Creators
Description
Highlights: •This paper studies the oxidation of Fe–6 at% Si alloy. •Oxidation has been done at 570 °C in 10−2 mbar for 300 h. •Silicon has been oxidized from the α-Fe–Si solid solution. •Wüstite, magnetite, and fayalite were detected. -- Abstract: Silicon has been oxidized from the α-Fe–Si solid solution during isothermal resistivity measurement at 570 °C. Measurements have been done in 10−2 mbar for 300 h. Mössbauer spectra showed that the α-FeSi solid solution, which is represented three sextets in Mössbauer spectra, was replaced by the pure iron (one sextet) after 168 h of heat treatment. Three new phases were obtained in the spectra representing wüstite (FeO), magnetite (Fe3O4) and fayalite (Fe2SiO4). These results were confirmed by X-ray and electron microscope measurements
Availability note (English)
Available from http://dx.doi.org/10.1016/j.jallcom.2013.03.073Additional details
Identifiers
- DOI
- 10.1016/j.jallcom.2013.03.073;
- PII
- S0925-8388(13)00604-X;
Publishing Information
- Journal Title
- Journal of Alloys and Compounds
- Journal Volume
- 567
- Journal Page Range
- p. 54-58
- ISSN
- 0925-8388
- CODEN
- JALCEU
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 45044112
- Subject category
- S36: MATERIALS SCIENCE;
- Descriptors DEI
- FERRITES; HEAT TREATMENTS; IRON OXIDES; IRON SILICATES; IRON SILICIDES; MAGNETITE; OXIDATION; SILICON; SILICON ALLOYS; SOLID SOLUTIONS; SPECTRA; SPECTROSCOPY; X RADIATION
- Descriptors DEC
- ALLOYS; CHALCOGENIDES; CHEMICAL REACTIONS; DISPERSIONS; ELECTROMAGNETIC RADIATION; ELEMENTS; FERRIMAGNETIC MATERIALS; HOMOGENEOUS MIXTURES; IONIZING RADIATIONS; IRON COMPOUNDS; IRON ORES; MAGNETIC MATERIALS; MATERIALS; MINERALS; MIXTURES; ORES; OXIDE MINERALS; OXIDES; OXYGEN COMPOUNDS; RADIATIONS; SEMIMETALS; SILICATES; SILICIDES; SILICON COMPOUNDS; SOLUTIONS; TRANSITION ELEMENT COMPOUNDS
Optional Information
- Copyright
- Copyright (c) 2013 Elsevier Science B.V., Amsterdam, The Netherlands, All rights reserved.