AC Susceptibility of the Dipolar Spin Ice Dy2Ti2O7: Experiments and Monte Carlo Simulations
arXiv:1305.1854 · doi:10.7566/JPSJ.82.104710
Abstract
Experimental data of the frequency-dependent ac susceptibility for the dipolar spin ice Dy2Ti2O7 has been analyzed by Monte Carlo simulations on the basis of the single-spin-flip Metropolis algorithm. We have directly evaluated the ac susceptibility by applying an ac magnetic field. We found that the simulated behaviors reproduces the experimental behavior of the ac susceptibility in the temperature range from 0.6 to 1.0 K, where dilute magnetic monopoles diffusively move. The conversion factor from simulation time to real time, i.e., the rate of hopping of monopoles to nearest-neighbor sites, strongly depends on temperature.
J. Phys. Soc. Jpn. 82, 104710 (2013)
References in corpus (8)
- Dirac Strings and Magnetic Monopoles in Spin Ice Dy2Ti2O7
- Low Temperature Spin Freezing in Dy2Ti2O7 Spin Ice
- Dy2Ti2O7 Spin Ice: a Test Case for Emergent Clusters in a Frustrated Magnet
- Kagomé ice state in the dipolar spin ice Dy_{2}Ti_{2}O_{7}
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Cited by in corpus (13)
- Magnetic Monopole Noise
- A Supercooled Spin Liquid State in the Frustrated Pyrochlore Dy2Ti2O7
- Phonon-mediated spin-flipping mechanism in the spin ices DyTiO and HoTiO
- Monopolar and dipolar relaxation in spin ice HoTiO
- Common Glass-Forming Spin-Liquid State in the Pyrochlore Magnets DyTiO and HoTiO
- Dipolar spin ice states with fast monopole hopping rate in CdErX (X = Se, S)
- Emergence of weak pyrochlore phase and signature of field induced spin ice ground state in DyLaZrO; x = 0, 0.15, 0.3
- Violation of the fluctuation-dissipation theorem and effective temperatures in spin ice
- Extremely slow non-equilibrium monopole dynamics in classical spin ice
- Slow spin dynamics and quantum tunneling of magnetization in the dipolar antiferromagnet DyScO
- Anomalous out-of-equilibrium dynamics in the spin-ice material DyTiO under moderate magnetic fields
- The monopole movement
- Universal dynamics of magnetic monopoles in two-dimensional kagomé ice