Phase Formation, Microstructure, and Permeability of Fe-Deficient Ni-Cu-Zn Ferrites (II): Effect of Oxygen Partial Pressure

We have investigated the phase formation, microstructure, and permeability of stoichiometric and Fe-deficient Ni-Cu-Zn ferrites of composition Ni<sub>0.30</sub>Cu<sub>0.20</sub>Zn<sub>0.50+z</sub>Fe<sub>2−z</sub>O<sub>4−(z/2)</sub> with 0 ≤...

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Main Authors: Christoph Priese, Jörg Töpfer
Format: Article
Language:English
Published: MDPI AG 2024-12-01
Series:Magnetochemistry
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Online Access:https://www.mdpi.com/2312-7481/10/12/97
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author Christoph Priese
Jörg Töpfer
author_facet Christoph Priese
Jörg Töpfer
author_sort Christoph Priese
collection DOAJ
description We have investigated the phase formation, microstructure, and permeability of stoichiometric and Fe-deficient Ni-Cu-Zn ferrites of composition Ni<sub>0.30</sub>Cu<sub>0.20</sub>Zn<sub>0.50+z</sub>Fe<sub>2−z</sub>O<sub>4−(z/2)</sub> with 0 ≤ z ≤ 0.06 sintered at 1000 °C in various oxygen partial pressures <i>p</i><sub>O2</sub>, which range from 0.21 atm down to 10<sup>−5</sup> atm. The density of the sintered samples is almost independent of the <i>p</i><sub>O2</sub>, whereas the grain size of the Fe-deficient ferrites decreases in more reducing atmospheres. Stoichiometric ferrites show a regular growth of single-phase ferrite grains if sintered in air. Sintering at <i>p</i><sub>O2</sub> ≤ 10<sup>−2</sup> atm leads to the formation of a small amount of Cu<sub>2</sub>O at grain boundaries and triple points. Fe-deficient compositions (z > 0) form Cu-poor stoichiometric ferrites, which coexist with a minority CuO phase homogeneously distributed between the grains after sintering in air. At <i>p</i><sub>O2</sub> ≤ 10<sup>−2</sup> atm, the CuO grain boundary phase starts to transform into Cu<sub>2</sub>O, which concentrates at some triple points at <i>p</i><sub>O2</sub> = 10<sup>−2</sup> atm, and it is more homogeneously distributed between the ferrite grains at the lower <i>p</i><sub>O2</sub>. Formation of the Cu oxide second phases is investigated using XRD, SEM, and EDX. The permeability at 1 MHz of the stoichiometric ferrites (z = 0) is between <i>µ</i>′ = 200 and <i>µ</i>′ = 300 within the studied range of the <i>p</i><sub>O2</sub>. The permeability at 1 MHz of the Fe-deficient samples decreases with the <i>p</i><sub>O2</sub>, e.g., from <i>µ</i>′ = 750 at <i>p</i><sub>O2</sub> = 0.21 atm to <i>µ</i>′ = 320 at <i>p</i><sub>O2</sub> = 10<sup>−5</sup> atm for z = 0.02, respectively.
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spelling doaj-art-ffdf9e26591346d4af6f47f6717dfd312025-08-20T02:51:00ZengMDPI AGMagnetochemistry2312-74812024-12-0110129710.3390/magnetochemistry10120097Phase Formation, Microstructure, and Permeability of Fe-Deficient Ni-Cu-Zn Ferrites (II): Effect of Oxygen Partial PressureChristoph Priese0Jörg Töpfer1Department SciTec, Ernst-Abbe-Hochschule Jena, 07745 Jena, GermanyDepartment SciTec, Ernst-Abbe-Hochschule Jena, 07745 Jena, GermanyWe have investigated the phase formation, microstructure, and permeability of stoichiometric and Fe-deficient Ni-Cu-Zn ferrites of composition Ni<sub>0.30</sub>Cu<sub>0.20</sub>Zn<sub>0.50+z</sub>Fe<sub>2−z</sub>O<sub>4−(z/2)</sub> with 0 ≤ z ≤ 0.06 sintered at 1000 °C in various oxygen partial pressures <i>p</i><sub>O2</sub>, which range from 0.21 atm down to 10<sup>−5</sup> atm. The density of the sintered samples is almost independent of the <i>p</i><sub>O2</sub>, whereas the grain size of the Fe-deficient ferrites decreases in more reducing atmospheres. Stoichiometric ferrites show a regular growth of single-phase ferrite grains if sintered in air. Sintering at <i>p</i><sub>O2</sub> ≤ 10<sup>−2</sup> atm leads to the formation of a small amount of Cu<sub>2</sub>O at grain boundaries and triple points. Fe-deficient compositions (z > 0) form Cu-poor stoichiometric ferrites, which coexist with a minority CuO phase homogeneously distributed between the grains after sintering in air. At <i>p</i><sub>O2</sub> ≤ 10<sup>−2</sup> atm, the CuO grain boundary phase starts to transform into Cu<sub>2</sub>O, which concentrates at some triple points at <i>p</i><sub>O2</sub> = 10<sup>−2</sup> atm, and it is more homogeneously distributed between the ferrite grains at the lower <i>p</i><sub>O2</sub>. Formation of the Cu oxide second phases is investigated using XRD, SEM, and EDX. The permeability at 1 MHz of the stoichiometric ferrites (z = 0) is between <i>µ</i>′ = 200 and <i>µ</i>′ = 300 within the studied range of the <i>p</i><sub>O2</sub>. The permeability at 1 MHz of the Fe-deficient samples decreases with the <i>p</i><sub>O2</sub>, e.g., from <i>µ</i>′ = 750 at <i>p</i><sub>O2</sub> = 0.21 atm to <i>µ</i>′ = 320 at <i>p</i><sub>O2</sub> = 10<sup>−5</sup> atm for z = 0.02, respectively.https://www.mdpi.com/2312-7481/10/12/97soft ferritesoxygen partial pressuremagnetic permeabilitypolycrystalline microstructure
spellingShingle Christoph Priese
Jörg Töpfer
Phase Formation, Microstructure, and Permeability of Fe-Deficient Ni-Cu-Zn Ferrites (II): Effect of Oxygen Partial Pressure
Magnetochemistry
soft ferrites
oxygen partial pressure
magnetic permeability
polycrystalline microstructure
title Phase Formation, Microstructure, and Permeability of Fe-Deficient Ni-Cu-Zn Ferrites (II): Effect of Oxygen Partial Pressure
title_full Phase Formation, Microstructure, and Permeability of Fe-Deficient Ni-Cu-Zn Ferrites (II): Effect of Oxygen Partial Pressure
title_fullStr Phase Formation, Microstructure, and Permeability of Fe-Deficient Ni-Cu-Zn Ferrites (II): Effect of Oxygen Partial Pressure
title_full_unstemmed Phase Formation, Microstructure, and Permeability of Fe-Deficient Ni-Cu-Zn Ferrites (II): Effect of Oxygen Partial Pressure
title_short Phase Formation, Microstructure, and Permeability of Fe-Deficient Ni-Cu-Zn Ferrites (II): Effect of Oxygen Partial Pressure
title_sort phase formation microstructure and permeability of fe deficient ni cu zn ferrites ii effect of oxygen partial pressure
topic soft ferrites
oxygen partial pressure
magnetic permeability
polycrystalline microstructure
url https://www.mdpi.com/2312-7481/10/12/97
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