Structural, magnetic properties, and hyperfine interactions of Ni0.8Cu0.1Zn0.1MoxFe2−2xO4 (0.0 ≤ x ≤ 0.1) nanospinel ferrites
Ni 0.8 Cu 0.1 Zn 0.1 Mo x Fe 2–2 x O 4 ( x ≤ 0.1) nanospinel ferrites (Mo → NiCuZn NSFs) were produced by sol–gel approach. A spinel structure formation with no impurities was confirmed by X-ray diffraction (XRD) patterns. The nanoparticles’ morphology and chemical composition of the products have...
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Veröffentlicht in: | Applied physics. A, Materials science & processing Materials science & processing, 2023-08, Vol.129 (8), Article 582 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | Ni
0.8
Cu
0.1
Zn
0.1
Mo
x
Fe
2–2
x
O
4
(
x
≤ 0.1) nanospinel ferrites (Mo → NiCuZn NSFs) were produced by sol–gel approach. A spinel structure formation with no impurities was confirmed by X-ray diffraction (XRD) patterns. The nanoparticles’ morphology and chemical composition of the products have been confirmed via SEM, TEM, HR-TEM, and EDX. By fitting Mössbauer spectra at RT, Hyperfine parameters were determined. A superparamagnetic state was observed in all samples. The Mo
4+
were found to reside in the B site mainly. Isomer shift values showed that Mössbauer spectra composed magnetic Fe
3+
sextets. Magnetic characteristics of Mo → NiCuZn NSFs are probed employing hysteresis loops at 300 K and 10 K. The significant role of Mo ions in the magnetic characteristics of the host material is revealed by employing saturation magnetization (
M
s
), magnetic moment (
n
B
), coercivity (
H
c
), SQR (squareness ratio), and magneto-crystalline anisotropy constant. While the samples show a superparamagnetic behavior at 300 K, they represent a magnetically soft material at 10 K. The magnetic parameters, with a minimum magnetization at
x
= 0.06, fluctuate with respect to Mo concentration at each temperature. The
M
s
and
n
B
become the maximum for the Mo → NiCuZn NSFs (
x
= 0.02) which yields the minimum
H
c
. The SQR is negligible at 300 K and low (much less than 0.5) at 10 K, reflecting the generation of multi-magnetic domains and a relatively low anisotropy field. |
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ISSN: | 0947-8396 1432-0630 |
DOI: | 10.1007/s00339-023-06867-9 |