Spin wave dispersion of ultra-low damping hematite ($\alpha\text{-Fe}_2\text{O}_3$) at GHz frequencies

TL;DR

This study demonstrates that hematite ($ ext{α-Fe}_2 ext{O}_3$), a natural mineral, exhibits ultra-low magnetic damping and high spin wave velocities at GHz frequencies, making it a promising sustainable material for magnonic devices.

Contribution

It provides the first detailed spin-wave dispersion analysis of hematite at GHz frequencies, highlighting its low damping and high group velocities as an alternative to garnet-based magnonics.

Findings

Damping coefficient of 1.1×10^{-5} at room temperature

Magnon group velocities of a few 10 km/s

Decay length of 1.1 cm in a 30 mT magnetic field

Abstract

Low magnetic damping and high group velocity of spin waves (SWs) or magnons are two crucial parameters for functional magnonic devices. Magnonics research on signal processing and wave-based computation at GHz frequencies focussed on the artificial ferrimagnetic garnet Y$_3$Fe$_5$O$_{12}$ (YIG) so far. We report on spin-wave spectroscopy studies performed on the natural mineral hematite ($\alpha\text{-Fe}_2\text{O}_3$) which is a canted antiferromagnet. By means of broadband GHz spectroscopy and inelastic light scattering, we determine a damping coefficient of $1.1\times10^{-5}$ and magnon group velocities of a few 10 km/s, respectively, at room temperature. Covering a large regime of wave vectors up to $k\approx 24~{\rm rad}/\mu$m, we find the exchange stiffness length to be relatively short and only about 1 \r{A}. In a small magnetic field of 30 mT, the decay length of SWs is estimated to be 1.1 cm similar to the best YIG. Still, inelastic light scattering provides surprisingly broad and partly asymmetric resonance peaks. Their characteristic shape is induced by the large group velocities, low damping and distribution of incident angles inside the laser beam. Our results promote hematite as an alternative and sustainable basis for magnonic devices with fast speeds and low losses based on a stable natural mineral.