Small-Scale Isotropy and Ramp-Cliff Structures in Scalar Turbulence

被引:29
作者
Buaria, Dhawal [1 ]
Clay, Matthew P. [2 ]
Sreenivasan, Katepalli R. [1 ,3 ,4 ]
Yeung, P. K. [2 ,5 ]
机构
[1] NYU, Tandon Sch Engn, New York, NY 11201 USA
[2] Georgia Inst Technol, Sch Aerosp Engn, Atlanta, GA 30332 USA
[3] NYU, Dept Phys, New York, NY 10012 USA
[4] NYU, Courant Inst Math Sci, New York, NY 10012 USA
[5] Georgia Inst Technol, Sch Mech Engn, Atlanta, GA 30332 USA
基金
美国国家科学基金会;
关键词
PASSIVE SCALARS; LOCAL ISOTROPY; FLUCTUATIONS; SKEWNESS;
D O I
10.1103/PhysRevLett.126.034504
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
Passive scalars advected by three-dimensional Navier-Stokes turbulence exhibit a fundamental anomaly in odd-order moments because of the characteristic ramp-cliff structures, violating small-scale isotropy. We use data from direct numerical simulations with grid resolution of up to 8192(3) at high Peclet numbers to understand this anomaly as the scalar diffusivity, D, diminishes, or as the Schmidt number, Sc = v/D, increases; here I. is the kinematic viscosity of the fluid. The microscale Reynolds number varies from 140 to 650 and Sc varies from 1 to 512. A simple model for the ramp-cliff structures is developed and shown to characterize the scalar derivative statistics very well. It accurately captures how the small-scale isotropy is restored in the large-Sc limit, and additionally suggests a possible correction to the Batchelor length scale as the relevant smallest scale in the scalar field.
引用
收藏
页数:6
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