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Simulation and validation of a spatially evolving turbulent boundary layer up to Reθ = 8300
KTH, Skolan för teknikvetenskap (SCI), Mekanik, Strömningsfysik. KTH, Skolan för teknikvetenskap (SCI), Centra, Linné Flow Center, FLOW. KTH, Centra, SeRC - Swedish e-Science Research Centre.
KTH, Skolan för teknikvetenskap (SCI), Mekanik, Strömningsfysik. KTH, Skolan för teknikvetenskap (SCI), Centra, Linné Flow Center, FLOW. KTH, Centra, SeRC - Swedish e-Science Research Centre.ORCID-id: 0000-0002-1663-3553
KTH, Skolan för teknikvetenskap (SCI), Mekanik, Stabilitet, Transition, Kontroll. KTH, Skolan för teknikvetenskap (SCI), Centra, Linné Flow Center, FLOW. KTH, Centra, SeRC - Swedish e-Science Research Centre.ORCID-id: 0000-0001-9627-5903
2014 (Engelska)Ingår i: International Journal of Heat and Fluid Flow, ISSN 0142-727X, E-ISSN 1879-2278, Vol. 47, s. 57-69Artikel i tidskrift (Refereegranskat) Published
Abstract [en]

Results of a finely resolved large-eddy simulation (LES) of a spatially developing zero-pressure-gradient turbulent boundary layer up to a Reynolds number of Reθ = 8300 are presented. The very long computational domain provides substantial assessment for suggested high Reynolds number (Re) trends. Statistics, integral quantities and spectral data are validated using high quality direct numerical simulation (DNS) ranging up to Reθ = 4300 and hot-wire measurements covering the remaining Re-range. The mean velocity, turbulent fluctuations, skin friction, and shape factor show excellent agreement with the reference data. Through utilisation of filtered DNS, subtle differences between the LES and DNS could to a large extent be explained by the reduced spanwise resolution of the LES. Spectra and correlations for the streamwise velocity and the wall-shear stress evidence a clear scale-separation and a footprint of large outer scales on the near-wall small scales. While the inner peak decreases in importance and reduces to 4% of the total energy at the end of the domain, the energy of the outer peak scales in outer units. In the near-wall region a clear k - 1 region emerges. Consideration of the two-dimensional spectra in time and spanwise space reveals that an outer time scale λt ≈ 10δ99 / U∞, with the boundary layer thickness δ99 and free-stream velocity U∞, is the correct scale throughout the boundary layer rather than the transformed streamwise wavelength multiplied by a (scale independent) convection velocity. Maps for the covariance of small scale energy and large scale motions exhibit a stronger linear Re dependence for the amplitude of the off-diagonal peak compared to the diagonal one, thereby indicating that the strength of the amplitude modulation can only qualitatively be assessed through the diagonal peak. In addition, the magnitude of the wall-pressure fluctuations confirms mixed scaling, and pressure spectra at the highest Re give a first indication of a -7/3 wave number dependence. © 2014 Elsevier Inc.

Ort, förlag, år, upplaga, sidor
2014. Vol. 47, s. 57-69
Nyckelord [en]
Large-eddy simulation, Numerical simulation, Turbulent boundary layers, Wall turbulence
Nationell ämneskategori
Strömningsmekanik och akustik
Identifikatorer
URN: urn:nbn:se:kth:diva-161020DOI: 10.1016/j.ijheatfluidflow.2014.02.006ISI: 000336773700006Scopus ID: 2-s2.0-84897381771OAI: oai:DiVA.org:kth-161020DiVA, id: diva2:794921
Forskningsfinansiär
Knut och Alice Wallenbergs StiftelseSwedish e‐Science Research Center
Anmärkning

QC 20150313

Tillgänglig från: 2015-03-13 Skapad: 2015-03-06 Senast uppdaterad: 2017-12-04Bibliografiskt granskad

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Örlü, RamisSchlatter, Philipp

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Eitel-Amor, GeorgÖrlü, RamisSchlatter, Philipp
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StrömningsfysikLinné Flow Center, FLOWSeRC - Swedish e-Science Research CentreStabilitet, Transition, Kontroll
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International Journal of Heat and Fluid Flow
Strömningsmekanik och akustik

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