Magnetic and Mössbauer Effect Study of Ca-Sc Co-doped M-Type Strontium Hexaferrite
The present study investigates the influence of Ca 2+ -Sc 3+ co-dpoing on the magnetic properties of Sr 1-x/12 Ca x/12 Fe 12-x Sc x O 19 ( x = 0.0 to 2.0) hexaferrites. The samples were prepared via a facile autocombustion technique followed by sintering in ambient air. X-ray powder diffraction patt...
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Veröffentlicht in: | Journal of superconductivity and novel magnetism 2021-10, Vol.34 (10), p.2551-2564 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | The present study investigates the influence of Ca
2+
-Sc
3+
co-dpoing on the magnetic properties of Sr
1-x/12
Ca
x/12
Fe
12-x
Sc
x
O
19
(
x
= 0.0 to 2.0) hexaferrites. The samples were prepared via a facile autocombustion technique followed by sintering in ambient air. X-ray powder diffraction patterns show the formation of the pure phase of M-type hexaferrite. The lattice parameters
a
and
c
increased with the Ca
2+
-Sc
3+
doping. The compounds’ magnetic properties were assessed as a function of temperature (10–300 K) and field (up to 6T). A rapid decline in room temperature coercivity from 5458 to 373 Oe and remanence value from 37 to 13 emu/g and a moderate decline in saturation magnetization from 76.9 to 57 emu/g were observed with increasing doping content from
x
= 0.0 to 2.0. The phase transition temperature, corresponding to ferrimagnetic to conical, was observed below 100 K, which disappeared at low doping content. The temperature-dependent behavior of magnetization and coercivity is discussed in view of spin non-collinearity due to the change in magnetic anisotropy. The Curie temperature dropped from 769 K at
x
= 0 to 568 K at the maximum substitution of
x
=2.0. The room temperature Mossbauer spectral analysis confirmed the preferred occupancy of Sc
3+
at the 4
f
2 site and the influence of Ca
2+
on the isomer shift values of the 2
b
site. The increased quadrupole shift values with the substitution implied distortion in 2
b
bipyramidal symmetry. The observed changes in magnetic properties and hyperfine parameters are ultimately tied to the preferred occupancy of Sc
3+
at the spin-down 4
f
2 site. |
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ISSN: | 1557-1939 1557-1947 |
DOI: | 10.1007/s10948-021-05882-2 |