TY - JOUR
T1 - Phase transitions in wave turbulence
AU - Vladimirova, Natalia
AU - Derevyanko, Stanislav
AU - Falkovich, Gregory
N1 - BSF; ISF; Minerva Foundation; German Ministry for education and research; [NSF PHYS-51164]We thank A. Zamolodchikov, V. Lebedev, E. Kats, A. Finkelstein, and B. Shraiman for helpful discussions. This research was supported by grants from the BSF, ISF, and by the Minerva Foundation, which is funded by the German Ministry for education and research. Part of the work was done at KITP, where it was supported by Grant No. NSF PHYS-51164. Computations were done at the New Mexico Computing Application Center.
PY - 2012/1/3
Y1 - 2012/1/3
N2 - We consider turbulence within the Gross-Pitaevsky model and look into the creation of a coherent condensate via an inverse cascade originating at small scales. The growth of the condensate leads to a spontaneous breakdown of statistical symmetries of overcondensate fluctuations: First, isotropy is broken, then a series of phase transitions marks the changing symmetry from twofold to threefold to fourfold. We describe respective anisotropic flux flows in the k space. At the highest level reached, we observe a short-range positional and long-range orientational order (as in a hexatic phase). In other words, the more one pumps the system, the more ordered the system becomes. The phase transitions happen when the system is pumped by an instability term and does not occur when pumped by a random force. We thus demonstrate nonuniversality of an inverse-cascade turbulence with respect to the nature of small-scale forcing.
AB - We consider turbulence within the Gross-Pitaevsky model and look into the creation of a coherent condensate via an inverse cascade originating at small scales. The growth of the condensate leads to a spontaneous breakdown of statistical symmetries of overcondensate fluctuations: First, isotropy is broken, then a series of phase transitions marks the changing symmetry from twofold to threefold to fourfold. We describe respective anisotropic flux flows in the k space. At the highest level reached, we observe a short-range positional and long-range orientational order (as in a hexatic phase). In other words, the more one pumps the system, the more ordered the system becomes. The phase transitions happen when the system is pumped by an instability term and does not occur when pumped by a random force. We thus demonstrate nonuniversality of an inverse-cascade turbulence with respect to the nature of small-scale forcing.
UR - http://www.scopus.com/inward/record.url?scp=84856301574&partnerID=8YFLogxK
U2 - 10.1103/PhysRevE.85.010101
DO - 10.1103/PhysRevE.85.010101
M3 - مقالة
C2 - 22400497
SN - 1539-3755
VL - 85
JO - Physical Review E
JF - Physical Review E
IS - 1
M1 - 010101
ER -