Published 1961
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Influence of a dipolar field on the nuclear resonance of iron-57 in an iron yttrium garnet (1961)
- 1. Commissariat a l'Energie Atomique, Saclay (France). Centre d'Etudes Nucleaires
Description
The existence of a dipolar magnetic field at the Fe3+ ion level in an iron-yttrium garnet makes it possible to explain the structure and the width of the nuclear resonance lines of Fe57 nuclei observed on the 16 a sites. (authors)
Availability note (English)
Available from INIS in electronic formAbstract (French)
L'existence d'un champ dipolaire magnetique au niveau des ions Fe3+ dans le grenat d'yttrium et de fer permet d'expliquer la structure et les largeurs des raies de resonance nucleaire des noyaux de 57Fe observees dans les sites 16 a. (auteurs)Files
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Additional details
Additional titles
- Original title (French)
- Influence du champ dipolaire sur la resonance nucleaire du fer-57 dans le grenat d'yttrium et de fer (1961)
Publishing Information
- Imprint Pagination
- 4 p.
- Report number
- CEA-R--2042
INIS
- Country of Publication
- France
- Country of Input or Organization
- France
- INIS RN
- 37121466
- Subject category
- S36: MATERIALS SCIENCE;
- Descriptors DEI
- BLOCH WALL; FERRITE GARNETS; IRON 57; IRON IONS; MAGNETIC DIPOLES; NUCLEAR MAGNETIC RESONANCE; YTTRIUM COMPOUNDS
- Descriptors DEC
- CHARGED PARTICLES; DIPOLES; DOMAIN STRUCTURE; EVEN-ODD NUCLEI; INTERMEDIATE MASS NUCLEI; IONS; IRON ISOTOPES; ISOTOPES; MAGNETIC RESONANCE; MINERALS; MULTIPOLES; NUCLEI; OXIDE MINERALS; RESONANCE; STABLE ISOTOPES; TRANSITION ELEMENT COMPOUNDS
Optional Information
- Notes
- 3 refs.