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Phys. Rev. E 76, 021124 (2007) [10 pages]

Conjugate field and fluctuation-dissipation relation for the dynamic phase transition in the two-dimensional kinetic Ising model

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D. T. Robb1,2,*, P. A. Rikvold1,3,4, A. Berger5, and M. A. Novotny6
1School of Computational Science, Florida State University, Tallahassee, Florida 32306, USA
2Department of Physics, Clarkson University, Potsdam, New York 13699, USA
3Center for Materials Research and Technology and Department of Physics, Florida State University, Tallahassee, Florida 32306, USA
4National High Magnetic Field Laboratory, Tallahassee, Florida 32310, USA
5San Jose Research Center, Hitachi Global Storage Technologies, San Jose, California 95120, USA
6Department of Physics and Astronomy and HPC2 Center for Computational Sciences, Mississippi State University, Mississippi State, Mississippi 39762, USA

Received 6 April 2007; published 30 August 2007

The two-dimensional kinetic Ising model, when exposed to an oscillating applied magnetic field, has been shown to exhibit a nonequilibrium, second-order dynamic phase transition (DPT), whose order parameter Q is the period-averaged magnetization. It has been established that this DPT falls in the same universality class as the equilibrium phase transition in the two-dimensional Ising model in zero applied field. Here we study the scaling of the dynamic order parameter with respect to a nonzero, period-averaged, magnetic “bias” field, Hb, for a DPT produced by a square-wave applied field. We find evidence that the scaling exponent, δd, of Hb at the critical period of the DPT is equal to the exponent for the critical isotherm, δe, in the equilibrium Ising model. This implies that Hb is a significant component of the field conjugate to Q. A finite-size scaling analysis of the dynamic order parameter above the critical period provides further support for this result. We also demonstrate numerically that, for a range of periods and values of Hb in the critical region, a fluctuation-dissipation relation (FDR), with an effective temperature Teff(T,P,H0) depending on the period, and possibly the temperature and field amplitude, holds for the variables Q and Hb. This FDR justifies the use of the scaled variance of Q as a proxy for the nonequilibrium susceptibility, Q⟩∕Hb, in the critical region.

© 2007 The American Physical Society

URL:
http://link.aps.org/doi/10.1103/PhysRevE.76.021124
DOI:
10.1103/PhysRevE.76.021124
PACS:
05.70.Ln, 64.60.Ht, 89.75.Da, 75.70.Cn

*Corresponding author. drobb@clarkson.edu