Moessbauer effect and electron spin resonance study of Cdsub(x)Mgsub(1-x)Fe2O4 system
- 1. Al-Azhar Univ., Cairo (Egypt). Faculty of Science
Description
This work deals with the application of Moessbauer Effect (ME) in studying the crystal electric field and the cation distribution among tetrahedral (A) and the octahedral (B) sites of the spinel structure in the ferrite system Cdsub(x)Mgsub(1-x)Fe2O4 (x = 0, 0.2,...1). The electron spin resonance technique (ESR) was also applied for studying this ferrite system. It was possible to characterize the ESR spectra of ferrite through the combination with the ME spectra. The complete site occupation with different types of cations was successfully achieved from the ME spectra. The values of the quadrupole splitting indicated that for each ferrite in the system there exists an electric field gradient surrounding the Fe3+ ions in each of the octahedral and tetrahedral sites. The increase in the Mg-concentration increases the symmetry of the electric field at these sites. (Auth.)
Additional details
Publishing Information
- Journal Title
- Hyperfine Interact.
- Journal Volume
- 28
- Journal Issue
- 1-4
- Series
- Hyperfine Interact.
- Journal Page Range
- 843-848
- ISSN
- 0304-3843
- CODEN
- HYIND
Conference
- Title
- International conference on the applications of the Moessbauer effect.
- Dates
- 16-20 Sep 1985.
- Place
- Leuven (Belgium).
INIS
- Country of Publication
- Netherlands
- Country of Input or Organization
- Switzerland
- INIS RN
- 17056180
- Subject category
- S75: CONDENSED MATTER PHYSICS, SUPERCONDUCTIVITY AND SUPERFLUIDITY;
- Resource subtype / Literary indicator
- Conference
- Descriptors DEI
- COMPARATIVE EVALUATIONS; CRYSTAL FIELD; ELECTRIC FIELDS; ELECTRON SPIN RESONANCE; FERRITES; HYPERFINE STRUCTURE; IRON 57; MOESSBAUER EFFECT; SPINELS
- Descriptors DEC
- EVALUATION; EVEN-ODD NUCLEI; FERRIMAGNETIC MATERIALS; INTERMEDIATE MASS NUCLEI; IRON ISOTOPES; ISOTOPES; MAGNETIC MATERIALS; MAGNETIC RESONANCE; MATERIALS; MINERALS; NUCLEI; OXIDE MINERALS; RESONANCE; STABLE ISOTOPES