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Related Experiment Videos

Double scaling and intermittency in shear dominated flows.

C M Casciola1, R Benzi, P Gualtieri

  • 1Dipartimento Meccanica e Aeronautica, Università di Roma "La Sapienza," Via Eudossiana 18, 00184, Roma, Italy.

Physical Review. E, Statistical, Nonlinear, and Soft Matter Physics
|January 22, 2002
PubMed
Summary

Intermittency in shear flows differs from isotropic turbulence due to Reynolds stresses. A new similarity law explains this, showing shear turbulence properties are fixed by the dissipation field.

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Area of Science:

  • Fluid Dynamics
  • Turbulence Research
  • Statistical Mechanics

Background:

  • Intermittency in turbulent flows is influenced by energy transfer, which is altered in shear-dominated conditions by Reynolds stresses.
  • Homogeneous and isotropic turbulence models do not fully capture the complexities of shear flows.
  • A refined similarity law is proposed to address the heightened intermittency observed in these flows.

Purpose of the Study:

  • To investigate the distinct nature of intermittency in shear-dominated flows compared to homogeneous and isotropic conditions.
  • To provide evidence for the coexistence of distinct inertial and shear-dominated ranges.
  • To theoretically predict scaling exponents in shear flows using insights from isotropic turbulence.

Main Methods:

  • Analysis of turbulent kinetic energy production and Reynolds stresses.

Related Experiment Videos

  • Application of a refined similarity law for intermittency.
  • Comparison of theoretical predictions with numerical and experimental data.
  • Examination of dissipation field properties and their influence on turbulent fluctuations.
  • Main Results:

    • Evidence supporting the coexistence of Kolmogorov-like inertial and shear-dominated ranges.
    • Demonstration that statistical properties of the dissipation field are largely insensitive to mean shear.
    • Accurate theoretical prediction of scaling exponents in the shear-dominated range.
    • Observation of universality in larger anisotropic scales of shear turbulence.

    Conclusions:

    • The study confirms the coexistence of two distinct regimes in shear flows.
    • The dissipation field's statistical properties are robust against mean shear, enabling predictions.
    • Larger anisotropic scales in shear turbulence exhibit universality, linking dissipation to fluctuation properties.