Abstract
We address a question which, after a decade-long discussion, still remains open: what is the nature of the ultraquantum regime of decay of quantum turbulence? The model developed in this work reproduces both the ultraquantum and the quasiclassical decay regimes and explains their hydrodynamical natures. In the case where turbulence is generated by forcing at some intermediate length scale, e.g., by the beam of vortex rings in the experiment of Walmsley and Golov [Phys. Rev. Lett. 100, 245301 (2008)], we explain the mechanisms of generation of both ultraquantum and quasiclassical regimes. We also find that the anisotropy of the beam is important for generating the large-scale motion associated with the quasiclassical regime.
- Received 3 January 2012
DOI:https://doi.org/10.1103/PhysRevB.85.060501
©2012 American Physical Society