Crystal structure and magnetic properties of the Y2.97Gd0.03Fe5−xLaxO12 compound: an experimental and theoretical investigation

In the present work, we have investigated the crystal structure and magnetic properties of the Y 2.97 Gd 0.03 Fe 5− x La x O 12 (Gd-La co-doped YIG) compound (0.00 ≤  x  ≤ 0.05) obtained by the citrate sol–gel method. Rietveld refinement of the X-ray diffraction patterns provided the lattice paramet...

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Veröffentlicht in:Journal of materials science 2024-09, Vol.59 (36), p.16884-16899
Hauptverfasser: Gonçalves, M., Matilla-Arias, J., Penha-Caland, J., Vilca-Huayhua, C., Coaquira, J. A. H., Guerrero, F., Guerra, Y., Viana, Bartolomeu C., Peña-Garcia, Ramón R.
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container_end_page 16899
container_issue 36
container_start_page 16884
container_title Journal of materials science
container_volume 59
creator Gonçalves, M.
Matilla-Arias, J.
Penha-Caland, J.
Vilca-Huayhua, C.
Coaquira, J. A. H.
Guerrero, F.
Guerra, Y.
Viana, Bartolomeu C.
Peña-Garcia, Ramón R.
description In the present work, we have investigated the crystal structure and magnetic properties of the Y 2.97 Gd 0.03 Fe 5− x La x O 12 (Gd-La co-doped YIG) compound (0.00 ≤  x  ≤ 0.05) obtained by the citrate sol–gel method. Rietveld refinement of the X-ray diffraction patterns provided the lattice parameter ( a ) values, which increased from 12.387(2) to 12.468(2) Å as the La 3+ content increased. Raman measurements confirmed the single-phase formation, whereas transmission electron microscopy (TEM) revealed elongated and irregular particles. The Mössbauer spectroscopy confirmed the presence of Fe 3+ and Fe 2+ cations and the coexistence of Fe 2+ and La 3+ cations in the octahedral and tetrahedral sites. Nonetheless, using a phenomenological model, it was suggested that the Fe 2+ and La 3+ ions tend to occupy preferentially the octahedral sites in the YIG structure. Further, the correspondence between the experimental and theoretically predicted saturation magnetization values indicated that the compound stoichiometry can be described by the chemical formula Y 3 + 2.97 Gd 3+ 0.03 Fe 3+ 5− x − y La 3+ x Fe 2+ y O 2− 12− y /2 . Magnetic parameters such as saturation magnetization, anisotropy constant, remanent magnetization, and coercive field values were computed and discussed as a function of cations distribution in the YIG crystal structure.
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The Mössbauer spectroscopy confirmed the presence of Fe 3+ and Fe 2+ cations and the coexistence of Fe 2+ and La 3+ cations in the octahedral and tetrahedral sites. Nonetheless, using a phenomenological model, it was suggested that the Fe 2+ and La 3+ ions tend to occupy preferentially the octahedral sites in the YIG structure. Further, the correspondence between the experimental and theoretically predicted saturation magnetization values indicated that the compound stoichiometry can be described by the chemical formula Y 3 + 2.97 Gd 3+ 0.03 Fe 3+ 5− x − y La 3+ x Fe 2+ y O 2− 12− y /2 . 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H.</au><au>Guerrero, F.</au><au>Guerra, Y.</au><au>Viana, Bartolomeu C.</au><au>Peña-Garcia, Ramón R.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Crystal structure and magnetic properties of the Y2.97Gd0.03Fe5−xLaxO12 compound: an experimental and theoretical investigation</atitle><jtitle>Journal of materials science</jtitle><stitle>J Mater Sci</stitle><date>2024-09-01</date><risdate>2024</risdate><volume>59</volume><issue>36</issue><spage>16884</spage><epage>16899</epage><pages>16884-16899</pages><issn>0022-2461</issn><eissn>1573-4803</eissn><abstract>In the present work, we have investigated the crystal structure and magnetic properties of the Y 2.97 Gd 0.03 Fe 5− x La x O 12 (Gd-La co-doped YIG) compound (0.00 ≤  x  ≤ 0.05) obtained by the citrate sol–gel method. Rietveld refinement of the X-ray diffraction patterns provided the lattice parameter ( a ) values, which increased from 12.387(2) to 12.468(2) Å as the La 3+ content increased. Raman measurements confirmed the single-phase formation, whereas transmission electron microscopy (TEM) revealed elongated and irregular particles. The Mössbauer spectroscopy confirmed the presence of Fe 3+ and Fe 2+ cations and the coexistence of Fe 2+ and La 3+ cations in the octahedral and tetrahedral sites. Nonetheless, using a phenomenological model, it was suggested that the Fe 2+ and La 3+ ions tend to occupy preferentially the octahedral sites in the YIG structure. Further, the correspondence between the experimental and theoretically predicted saturation magnetization values indicated that the compound stoichiometry can be described by the chemical formula Y 3 + 2.97 Gd 3+ 0.03 Fe 3+ 5− x − y La 3+ x Fe 2+ y O 2− 12− y /2 . Magnetic parameters such as saturation magnetization, anisotropy constant, remanent magnetization, and coercive field values were computed and discussed as a function of cations distribution in the YIG crystal structure.</abstract><cop>New York</cop><pub>Springer US</pub><doi>10.1007/s10853-024-10209-2</doi><tpages>16</tpages><orcidid>https://orcid.org/0000-0002-4945-1297</orcidid></addata></record>
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subjects Anisotropy
Cations
Ceramics
Characterization and Evaluation of Materials
Chemistry and Materials Science
citrates
Classical Mechanics
Coercivity
Crystal structure
Crystallography and Scattering Methods
Diffraction patterns
Elongated structure
Ferrous ions
Gadolinium
Irregular particles
Magnetic properties
Magnetic saturation
magnetism
Materials Science
Mossbauer spectroscopy
Parameters
Polymer Sciences
Sol-gel processes
sol-gel processing
Solid Mechanics
spectroscopy
Stoichiometry
transmission electron microscopy
X-ray diffraction
title Crystal structure and magnetic properties of the Y2.97Gd0.03Fe5−xLaxO12 compound: an experimental and theoretical investigation
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