Turbulent kinetic energy balance of an oscillatory boundary layer in the transition to the fully turbulent regime

Francisco Pedocchi, Mariano I. Cantero, Marcelo H. García

Research output: Contribution to journalArticlepeer-review

Abstract

The sinusoidal oscillation of a fluid in the vicinity of a rigid smooth wall is studied using the results of direct numerical simulation of the Navier-Stokes equations. Simulations are performed at a wave Reynolds number Rew = UmaxA/ν = 1.41 × 106 in the turbulent regime. The computed statistics are compared with great success with the available experimental results reported in the literature for Umax = 1.02 m/s the maximum orbital velocity, A = 1.58 m the amplitude of the water excursion, and ν = 1.14 × 106 m2/s the kinematic viscosity of the fluid (Rew = UmaxA/ν = 1.41 × 106). The simulation results allow to identify the development of an unsteady shear layer and regions of zero and negative turbulent kinetic energy (TKE) production. The TKE balance is studied in detail, analyzing the role of each of the terms in the balance equation and the relative relevance of different TKE transport mechanisms. It is found that the local derivative of the TKE is particularly important in the shear layer region. The present results provide an accurate and detailed dataset that could be used for validation of both analytical and numerical models of oscillatory boundary layer flows.

Original languageEnglish (US)
Article numberN32
Pages (from-to)1-27
Number of pages27
JournalJournal of Turbulence
Volume12
DOIs
StatePublished - 2011

Keywords

  • Direct numerical simulation
  • Oscillatory boundary layer
  • Turbulent kinetic energy balance

ASJC Scopus subject areas

  • Computational Mechanics
  • Condensed Matter Physics
  • Mechanics of Materials
  • General Physics and Astronomy

Fingerprint

Dive into the research topics of 'Turbulent kinetic energy balance of an oscillatory boundary layer in the transition to the fully turbulent regime'. Together they form a unique fingerprint.

Cite this