The permittivity and permeability measurements of ferric oxide (Fe
2O
3) were carried out over a broad temperature range from 24°C to above 1000°C at 915 and 2450 MHz. The real part and imaginary part of complex relative permittivity (
εr′ and
εr″) of ferric oxide slightly increase with temperature below 450°C, above which
εr′ increases significantly while
εr″ presents a broad dielectric loss peak between 450 and 1000°C. Contrary to
εr′ and
εr″, the real part and imaginary part of complex relative permeability (
μr′ and
μr″) remain relatively invariable (1 and 0, respectively) until 700°C. The
μr′ values subsequently exhibit a decreasing tendency due to the increased electrical conductivity at higher temperatures while the
μr″ values stay negligible as temperature increases. The results demonstrate that the dielectric loss is the primary factor contributing to microwave absorption of Fe
2O
3. The calculation of microwave penetration depth shows that Fe
2O
3 undergoes a transition from a microwave transparent material to a good microwave absorber with increasing temperature.
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