Structural and low-temperature magnetic studies on compounds Sm2Fe17 with aluminium substitution for iron
Creators
- 1. Oregon Graduate Center, Beaverton (USA)
- 2. California Univ., La Jolla, San Diego (USA). Dept. of Chemistry
Description
Aluminium substitution for iron in Sm2Fe17results in stabilization of the Th2Zn17structure. Compounds are homogeneous from x=0.20 to x=0.50 in Smsub(0.105)Fesub(0.895-x)Alsub(x) when annealed at 8000C. In this structure, Fe and Al are statistically distributed on 6(c), 9(d), 18(f) and 18(h) sites. Materials with x=0-0.15 are composed of the Th2Zn17type and Fe. The magnetic hardness at cryogenic temperatures increases rapidly around a composition with x=0.30. A value of coercive force, Hsub(c)=15kOe, is obtained both on bulk and powder material with x=0.50 at 4.2K. This low-temperature magnetic hardness appears to be connected with the presence of highly energetic domain walls. The mechanism of demagnetization involves domain nucleation, in contrast with Smsub(0.167)Cosub(0.833-x)Alsub(x) where demagnetization is predominantly governed by domain wall pinning. (Auth.)
Additional details
Identifiers
Publishing Information
- Journal Title
- Journal of the Less Common Metals
- Journal Volume
- 44
- Series
- J. Less-Common Met.
- Journal Page Range
- 183-193
- ISSN
- 0022-5088
INIS
- Country of Publication
- Switzerland
- Country of Input or Organization
- Switzerland
- INIS RN
- 7244110
- Subject category
- S36: MATERIALS SCIENCE;
- Descriptors DEI
- ALUMINIUM ALLOYS; CURIE POINT; DOMAIN STRUCTURE; IRON ALLOYS; LATTICE PARAMETERS; MAGNETIC PROPERTIES; SAMARIUM ALLOYS; ULTRALOW TEMPERATURE; X-RAY DIFFRACTION
- Descriptors DEC
- ALLOYS; COHERENT SCATTERING; DIFFRACTION; PHYSICAL PROPERTIES; RARE EARTH ALLOYS; SCATTERING; THERMODYNAMIC PROPERTIES; TRANSITION ELEMENT ALLOYS; TRANSITION TEMPERATURE
Optional Information
- Notes
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