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Dynamics of three-dimensional turbulence from Navier-Stokes equations

Katepalli R. Sreenivasan and Victor Yakhot
Phys. Rev. Fluids 6, 104604 – Published 15 October 2021

Abstract

In statistically homogeneous and isotropic turbulence, the average value of the velocity increment δru=u(x+r)u(x), where x and x+r are two positions in the flow and u is the velocity in the direction of the separation distance r, is identically zero, and so to characterize the dynamics one often uses the Reynolds number based on (δru)2, which acts as the coupling constant for scale-to-scale interactions. This description can be generalized by introducing structure functions of order n, Sn=(δru)n, which allow one to probe velocity increments including rare and extreme events, by considering δru(n)=O(Sn1/n) for large and small n. If Snrζn, the theory for the anomalous exponents ζn in the entire allowable interval 1<n< is one of the long-standing challenges in turbulence (one takes absolute values of δru for negative n), usually attacked by various qualitative cascade models. We accomplish two major tasks here. First, we show that the turbulent microscale Reynolds number RλT (based on a suitably defined turbulent viscosity) is 8.8 in the inertial range with anomalous scaling, when the standard microscale Reynolds number Rλ (defined using normal viscosity) exceeds that same number (which in practice could be by a large factor). When the normal and turbulent microscale Reynolds numbers become equal to or fall below 8.8, the anomaly disappears in favor of Gaussian statistics. Conversely, if one starts with a Gaussian state and increases Rλ beyond 8.8, one ushers in the anomalous scaling; the inference is that RλT8.8 and remains constant at that value with further increase in Rλ. Second, we derive expressions for the anomalous scaling exponents of structure functions and moments of spatial derivatives, by analyzing the Navier-Stokes equations in the form developed by Hopf. We present a novel procedure to close the Hopf equation, resulting in expressions for ζn in the entire range of allowable moment order n, and demonstrate that accounting for the temporal dynamics changes the scaling from normal to anomalous. For large n, the theory predicts the saturation of ζn with n, leading to several inferences, two among which are (a) the smallest length scale ηn=LRe1LRe3/4, where Re is the large-scale Reynolds number, and (b) that velocity excursions across even the smallest length scales can sometimes be as large as the large-scale velocity itself. Theoretical predictions for each of these aspects are shown to be in excellent quantitative agreement with available experimental and numerical data.

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  • Received 11 June 2021
  • Accepted 15 September 2021

DOI:https://doi.org/10.1103/PhysRevFluids.6.104604

©2021 American Physical Society

Physics Subject Headings (PhySH)

  1. Research Areas
Nonlinear DynamicsFluid DynamicsStatistical Physics & Thermodynamics

Authors & Affiliations

Katepalli R. Sreenivasan1,* and Victor Yakhot2,1,†

  • 1Department of Mechanical and Aerospace Engineering, Courant Institute of Mathematical Sciences, and Department of Physics, New York University, New York 11201, USA
  • 2Department of Mechanical Engineering, Boston University, Boston, Massachusetts 02215, USA

  • *krs3@nyu.edu
  • vy@bu.edu

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Vol. 6, Iss. 10 — October 2021

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