1951
DOI: 10.1051/jphysrad:01951001203024900
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Aimantation spontanée des ferrites

Abstract: HAL is a multi-disciplinary open access archive for the deposit and dissemination of scientific research documents, whether they are published or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers. L'archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d'enseignement et de recherche français ou étrangers, des labor… Show more

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Cited by 137 publications
(26 citation statements)
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“…It is significantly lower. Note that 5k-M sat of CoF Ac is higher than that reported for bulk CoFe 2 O 4 (93.9 emu g À 1 [6]). …”
Section: Resultscontrasting
confidence: 53%
“…It is significantly lower. Note that 5k-M sat of CoF Ac is higher than that reported for bulk CoFe 2 O 4 (93.9 emu g À 1 [6]). …”
Section: Resultscontrasting
confidence: 53%
“…However, even for the case of bulk samples, it has been possible to obtain much larger value of magnetisation by quenching. These values were obtained by extrapolating to 0 K. Pauthenet and Bochirol [7] have reported an increase in 0 K saturation magnetisation for bulk MgFe 2 O 4 by quenching them from 1200°C (61 emu/g). Kriessman and Harrison have demonstrated a further increase in 0 K magnetisation up to 63 emu/g by quenching from 1400°C [8].…”
Section: Discussionmentioning
confidence: 99%
“…Magnesium ferrite is an interesting ferrite because of change in its properties due to thermal treatment [7,8]. There have been various reports on the enhancement of magnetisation of magnesium ferrite when quenched from higher temperatures.…”
Section: Introductionmentioning
confidence: 99%
“…However, the principal magnetic mineral in the sills at Site 857 is nearly pure magnetite, with Curie temperature of 580°C. The spontaneous magnetization of pure magnetite at 300°C is lowered by about 20% compared to the roomtemperature value (Panthenet, 1952). Because the magnetite in the sills is in the pseudo-single-domain range, the in-situ intensity of remanent magnetization is lowered by roughly the same degree as the spontaneous magnetization (McClelland and Sugiura, 1987).…”
Section: Origin Of the Subdued Marine Magnetic Anomalies Over Middle mentioning
confidence: 92%