Abstract
While a clean, driven system generically absorbs energy until it reaches “infinite temperature,” it may do so very slowly exhibiting what is known as a prethermal regime. Here, we show that the emergence of an additional approximately conserved quantity in a periodically driven (Floquet) system can give rise to an analogous long-lived regime. This can allow for nontrivial dynamics, even from initial states that are at a high or infinite temperature with respect to an effective Hamiltonian governing the prethermal dynamics. We present concrete settings with such a prethermal regime, one with a period-doubled (time-crystalline) response. We also present a direct diagnostic to distinguish this prethermal phenomenon from its infinitely long-lived many-body localized cousin. We apply these insights to a model of the recent NMR experiments by Rovny et al. [Phys. Rev. Lett. 120, 180603 (2018)] which, intriguingly, detected signatures of a Floquet time crystal in a clean three-dimensional material. We show that a mild but subtle variation of their driving protocol can increase the lifetime of the time-crystalline signal by orders of magnitude.
- Received 16 October 2019
- Revised 25 January 2020
- Accepted 6 March 2020
DOI:https://doi.org/10.1103/PhysRevX.10.021046
Published by the American Physical Society under the terms of the Creative Commons Attribution 4.0 International license. Further distribution of this work must maintain attribution to the author(s) and the published article’s title, journal citation, and DOI. Open access publication funded by the Max Planck Society.
Published by the American Physical Society
Physics Subject Headings (PhySH)
Popular Summary
The periodic driving of quantum systems can reveal novel properties and phenomena. A case in point is the discovery of new states of matter known as time crystals, which exhibit ever-changing behavior that repeats in time. A major obstacle toward realizing these phases is the tendency of driven systems to heat up toward featureless infinite temperature states. One strategy to circumvent this behavior is to delay the onset of heating by engineering a long-lived transient “prethermal” regime. We present a new mechanism for getting a prethermal regime via an additional approximate conservation law such as the total magnetization of the system. This can allow for prethermal regimes in a larger class of systems, such as those that may already be at high or infinite temperature, a phenomenon we call prethermalization without temperature.
We use our framework to explain long-lived time-crystalline signatures in a recent experimental setup of nuclear magnetic resonance spins, a system that falls outside previously known mechanisms to prevent or delay thermalization. We also predict that a judiciously chosen magnetic field can enhance the lifetime of the prethermal time crystal in the nuclear magnetic resonance setup by several orders of magnitude.
Finally, while many experiments are under way to search for and understand time crystals, they are inherently limited in their observation timescales. Therefore, it is crucial to investigate theoretically how to distinguish infinitely long-lived time crystals from transient prethermal versions. We show that local autocorrelation functions evaluated from a wide range of initial states can serve that purpose.
In all, our results extend frameworks for obtaining long-lived prethermal regimes, shed light on current experiments, and provide a way to tell long-lived time crystals from prethermal ones while also showing a clear experimental pathway toward optimization of time-crystal lifetimes.