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Investigation of (R1-xR'x)2(Fe,Co)17 powders by Mössbauer spectrometry

Identifieur interne : 000088 ( PascalFrancis/Checkpoint ); précédent : 000087; suivant : 000089

Investigation of (R1-xR'x)2(Fe,Co)17 powders by Mössbauer spectrometry

Auteurs : F. Richomme [France] ; J. M. Le Breton [France] ; M. S. Ben Kraiem [Tunisie] ; A. Cheikhrouhou [Tunisie]

Source :

RBID : Pascal:10-0383238

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English descriptors

Abstract

We investigated (R1-xR'x)2Fe17 and (R1-xR'x)2Fe16Co powders by 57Fe Mössbauer spectrometry at 295 K where R and R' are Y, Nd, Sm, Gd. The spectra of the (R1-xR'x)2Fe17 compounds have been fitted with seven sextets: 18f12, 18f6, 18h12, 18h6, 9d6, 9d3 and 6c. The isomer shifts of the different Fe sites are in agreement with the Wigner-Seitz cell volumes. They do not depend on the nature of the rare earth. The hyperfine fields are consistent with the evolution of the Curie temperature. To account for substitution effects due to the partial replacement of Fe by Co, the Mössbauer spectra of the (R1-xR'x)2Fe16Co samples have been fitted with four sextets corresponding to the 18f, 18h, 9d, and 6c Fe sites, by considering the site occupancy of the Co atoms in the lattice. The evolution of the hyperfine field with the rare-earth concentration is discussed and interpreted in relation with the magnetic coupling between rare-earth and Fe magnetic sublattices, in agreement with previous magnetic measurements.


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Pascal:10-0383238

Le document en format XML

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(Fe,Co)
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powders by Mössbauer spectrometry</title>
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<title xml:lang="en" level="a">Investigation of (R
<sub>1-x</sub>
R'
<sub>x</sub>
)
<sub>2</sub>
(Fe,Co)
<sub>17</sub>
powders by Mössbauer spectrometry</title>
<author>
<name sortKey="Richomme, F" sort="Richomme, F" uniqKey="Richomme F" first="F." last="Richomme">F. Richomme</name>
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<s1>Groupe de Physique des Matériaux, UMR CNRS 6634</s1>
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<sZ>2 aut.</sZ>
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<name sortKey="Ben Kraiem, M S" sort="Ben Kraiem, M S" uniqKey="Ben Kraiem M" first="M. S." last="Ben Kraiem">M. S. Ben Kraiem</name>
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<term>Cobalt alloys</term>
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<term>Isomer shift</term>
<term>Line splitting</term>
<term>Magnetization</term>
<term>Moessbauer effect</term>
<term>Rare earth alloys</term>
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<div type="abstract" xml:lang="en">We investigated (R
<sub>1-x</sub>
R'
<sub>x</sub>
)
<sub>2</sub>
Fe
<sub>17</sub>
and (R
<sub>1-x</sub>
R'
<sub>x</sub>
)
<sub>2</sub>
Fe
<sub>16</sub>
Co powders by
<sup>57</sup>
Fe Mössbauer spectrometry at 295 K where R and R' are Y, Nd, Sm, Gd. The spectra of the (R
<sub>1-x</sub>
R'
<sub>x</sub>
)
<sub>2</sub>
Fe
<sub>17</sub>
compounds have been fitted with seven sextets: 18f
<sub>12</sub>
, 18f
<sub>6</sub>
, 18h
<sub>12</sub>
, 18h
<sub>6</sub>
, 9d
<sub>6</sub>
, 9d
<sub>3</sub>
and 6c. The isomer shifts of the different Fe sites are in agreement with the Wigner-Seitz cell volumes. They do not depend on the nature of the rare earth. The hyperfine fields are consistent with the evolution of the Curie temperature. To account for substitution effects due to the partial replacement of Fe by Co, the Mössbauer spectra of the (R
<sub>1-x</sub>
R'
<sub>x</sub>
)
<sub>2</sub>
Fe
<sub>16</sub>
Co samples have been fitted with four sextets corresponding to the 18f, 18h, 9d, and 6c Fe sites, by considering the site occupancy of the Co atoms in the lattice. The evolution of the hyperfine field with the rare-earth concentration is discussed and interpreted in relation with the magnetic coupling between rare-earth and Fe magnetic sublattices, in agreement with previous magnetic measurements.</div>
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<s1>Investigation of (R
<sub>1-x</sub>
R'
<sub>x</sub>
)
<sub>2</sub>
(Fe,Co)
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powders by Mössbauer spectrometry</s1>
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<s0>We investigated (R
<sub>1-x</sub>
R'
<sub>x</sub>
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<sub>2</sub>
Fe
<sub>17</sub>
and (R
<sub>1-x</sub>
R'
<sub>x</sub>
)
<sub>2</sub>
Fe
<sub>16</sub>
Co powders by
<sup>57</sup>
Fe Mössbauer spectrometry at 295 K where R and R' are Y, Nd, Sm, Gd. The spectra of the (R
<sub>1-x</sub>
R'
<sub>x</sub>
)
<sub>2</sub>
Fe
<sub>17</sub>
compounds have been fitted with seven sextets: 18f
<sub>12</sub>
, 18f
<sub>6</sub>
, 18h
<sub>12</sub>
, 18h
<sub>6</sub>
, 9d
<sub>6</sub>
, 9d
<sub>3</sub>
and 6c. The isomer shifts of the different Fe sites are in agreement with the Wigner-Seitz cell volumes. They do not depend on the nature of the rare earth. The hyperfine fields are consistent with the evolution of the Curie temperature. To account for substitution effects due to the partial replacement of Fe by Co, the Mössbauer spectra of the (R
<sub>1-x</sub>
R'
<sub>x</sub>
)
<sub>2</sub>
Fe
<sub>16</sub>
Co samples have been fitted with four sextets corresponding to the 18f, 18h, 9d, and 6c Fe sites, by considering the site occupancy of the Co atoms in the lattice. The evolution of the hyperfine field with the rare-earth concentration is discussed and interpreted in relation with the magnetic coupling between rare-earth and Fe magnetic sublattices, in agreement with previous magnetic measurements.</s0>
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<s5>08</s5>
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