Abstract

The magnetic nature of layered chromium perovskites, Srn+1CrnO3n+1 (n = 1–3) was studied by μ+SR using powder samples prepared by a high pressure synthesis technique. According to the weak transverse field measurements, each sample entered a magnetically ordered state below 110, 200, and 90 K for the n = 1, 2, and 3 samples, respectively. Zero field (ZF) spectra below the transition temperature exhibited a clear oscillation due to the formation of quasi-static magnetic order. The Fourier transform frequency-spectrum for the ZF time-spectrum indicated the existence of the multiple oscillation components. The frequencies for the multiple oscillatory signals showed a complex temperature dependence, implying the occurrence of structural change/transitions below TN.

Keywords:
Chromium Materials science Physics Analytical Chemistry (journal) Mineralogy Chemistry Metallurgy

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3
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0.31
FWCI (Field Weighted Citation Impact)
6
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0.61
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Citation History

Topics

Advanced Condensed Matter Physics
Physical Sciences →  Physics and Astronomy →  Condensed Matter Physics
Magnetic and transport properties of perovskites and related materials
Physical Sciences →  Materials Science →  Electronic, Optical and Magnetic Materials
Nuclear materials and radiation effects
Physical Sciences →  Materials Science →  Materials Chemistry

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