Persistent dynamic magnetic state in artificial honeycomb spin ice

J. Guo, P. Ghosh, D. Hill, Y. Chen, L. Stingaciu, P. Zolnierczuk, C. A. Ullrich, D. K. Singh

Research output: Contribution to journalArticlepeer-review

1 Scopus citations

Abstract

Topological magnetic charges, arising due to the non-vanishing magnetic flux on spin ice vertices, serve as the origin of magnetic monopoles that traverse the underlying lattice effortlessly. Unlike spin ice materials of atomic origin, the dynamic state in artificial honeycomb spin ice is conventionally described in terms of finite size domain wall kinetics that require magnetic field or current application. Contrary to this common understanding, here we show that a thermally tunable artificial permalloy honeycomb lattice exhibits a perpetual dynamic state due to self-propelled magnetic charge defect relaxation in the absence of any external tuning agent. Quantitative investigation of magnetic charge defect dynamics using neutron spin echo spectroscopy reveals sub-ns relaxation times that are comparable to the relaxation of monopoles in bulk spin ices. Most importantly, the kinetic process remains unabated at low temperature where thermal fluctuation is negligible. This suggests that dynamic phenomena in honeycomb spin ice are mediated by quasi-particle type entities, also confirmed by dynamic Monte-Carlo simulations that replicate the kinetic behavior. Our research unveils a macroscopic magnetic particle that shares many known traits of quantum particles, namely magnetic monopole and magnon.

Original languageEnglish
Article number5212
JournalNature Communications
Volume14
Issue number1
DOIs
StatePublished - Dec 2023

Funding

We thank Valeria Lauter and George Yumnam for helping us understand the magnetic charge distribution on honeycomb vertices. We also thank Antonio Faraone and Georg Ehlers for the helpful discussion on the use of the NSE technique in probing magnetic materials and designing the experiment. This work was supported by the U.S. Department of Energy, Office of Science, Basic Energy Sciences under Awards No. DE-SC0014461 (DKS) and DE-SC0019109 (CAU). This work utilized the facilities supported by the Office of Basic Energy Sciences, US Department of Energy.

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