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Bernard Gillot

Researcher at Centre national de la recherche scientifique

Publications -  93
Citations -  1419

Bernard Gillot is an academic researcher from Centre national de la recherche scientifique. The author has contributed to research in topics: Spinel & Manganese. The author has an hindex of 22, co-authored 93 publications receiving 1370 citations.

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Particle size effects on the oxidation–reduction behavior of Mn3O4 hausmannite

TL;DR: In this paper, the oxidation of hausmannite, Mn3O4, of different particle sizes has been studied by thermogravimetry with a large range of linear heating programs under an oxygen pressure of 10 5 Pa for high heating rate (600C/h) and whatever the particle size, Mn 3O4 was converted to a-Mn2O3.
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Influence of crystallite size on the oxidation kinetics of magnetite

TL;DR: In this article, the oxidation of magnetite yields the lacunar phase γ-Fe 2 O 3, for sizes less than 5000 A, and the rhombohedral phase, α-Fe 3 O 3 for sizes above 10 000 A.
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Infrared studies on the behavior in oxygen of cobalt-substituted magnetites: Comparison with zinc-substituted magnetites

TL;DR: In this paper, the spectral properties of cobalt-substituted magnetites (Fe3+)A(Co2+xFe2+1−xFe3+,BO2−4, pretreated in oxygen) were investigated as a function of temperature.
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Cation valencies and distribution in the spinels CoxCuyMnzFeuO4+δ (δ≥0) thin films studied by X-ray photoelectron spectroscopy

TL;DR: In this article, X-ray photoelectron spectroscopy has been used to elucidate the valencies and cation distribution of the copper and manganese in the spinels Co x Cu y Mn z Fe u O 4+ δ ( δ ≥ 0) as thin films prepared by r.f. sputtering on glass substrates.
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Etude de la cinetique d'oxydation de magnetites finement divisees. I - Influence de la substitution par l'aluminium

TL;DR: In this article, the kinetics of substitution magnetites oxidation into metastable phase γ (Fe 3+ 1−y Al 3+ y ) 2 O 3 (x = 3y) has been accounted for by means of the law of diffusion, under variable working conditions, of the cationic vacancies generated at solid-gas interface with a diffusion coefficient that decreases when the stoichiometric difference is high.