Wall turbulence without walls

Mizuno, Yoshinori and Jiménez Sendín, Javier ORCID: https://orcid.org/0000-0003-0755-843X (2013). Wall turbulence without walls. "Journal of Fluid Mechanics", v. 723 ; pp. 429-455. ISSN 00221120. https://doi.org/10.1017/jfm.2013.137.

Descripción

Título: Wall turbulence without walls
Autor/es:
Tipo de Documento: Artículo
Título de Revista/Publicación: Journal of Fluid Mechanics
Fecha: 1 Abril 2013
ISSN: 00221120
Volumen: 723
Materias:
ODS:
Palabras Clave Informales: Boundary-Layers; Channel Flow; Direct Numerical-Simulation; High-Reynolds-Number; Large-Eddy Simulations; Large-Scale; Outer Layer; Pipe-Flow; Rough Walls; Structural Similarity; Turbulence Simulation; Turbulent Boundary Layers; Turbulent Flows
Escuela: E.T.S. de Ingeniería Aeronáutica y del Espacio (UPM)
Departamento: Mecánica de Fluidos y Propulsión Aeroespacial
Licencias Creative Commons: Reconocimiento - Sin obra derivada - No comercial

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Resumen

We perform direct numerical simulations of turbulent channels whose inner layer is replaced by an off-wall boundary condition synthesized from a rescaled interior flow plane. The boundary condition is applied within the logarithmic layer, and mimics the linear dependence of the length scales of the velocity fluctuations with respect to the distance to the wall. The logarithmic profile of the mean streamwise velocity is recovered, but only if the virtual wall is shifted to a position different from the location assumed by the boundary condition. In those shifted coordinates, most flow properties are within 5-10% of full simulations, including the Karman constant, the fluctuation intensities, the energy budgets and the velocity spectra and correlations. On the other hand, buffer-layer structures do not form, including the near-wall energy maximum, and the velocity fluctuation profiles are logarithmic, strongly suggesting that the logarithmic layer is essentially independent of the near-wall dynamics. The same agreement holds when the technique is applied to large-eddy simulations. The different errors are analysed, especially the reasons for the shifted origin, and remedies are proposed. It is also shown that the length rescaling is required for a stationary logarithmic-like layer. Otherwise, the flow evolves into a state resembling uniformly sheared turbulence.

Proyectos asociados

Tipo
Código
Acrónimo
Responsable
Título
Gobierno de España
TRA2006-08226
Sin especificar
Sin especificar
Sin especificar
Gobierno de España
TRA2009-11498
Sin especificar
Sin especificar
Sin especificar

Más información

ID de Registro: 88144
Identificador DC: https://oa.upm.es/88144/
Identificador OAI: oai:oa.upm.es:88144
URL Portal Científico: https://portalcientifico.upm.es/es/ipublic/item/5488492
Identificador DOI: 10.1017/jfm.2013.137
URL Oficial: https://www.cambridge.org/core/journals/journal-of...
Depositado por: iMarina Portal Científico
Depositado el: 04 Mar 2025 10:59
Ultima Modificación: 12 Mar 2025 12:00