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Showing papers by "Juan C. del Álamo published in 2003"


Journal ArticleDOI
TL;DR: In this paper, the spectra of numerically simulated channels at Reτ = 180 and Reτ=550 in very large boxes are described and analyzed, and they support a model in which the u-structures can be decomposed in two components.
Abstract: The spectra of numerically simulated channels at Reτ=180 and Reτ=550 in very large boxes are described and analyzed. They support a model in which the u-structures can be decomposed in two components. The first one is formed by structures of size λx≳5 h, λz≈2 h, which span most of the channel height, and penetrate into the buffer layer. The second one has maximum intensity in the near-wall region, where it is highly anisotropic and scales in inner units. It widens, lengthens, and becomes more isotropic in the outer layer, where it scales with h. The cospectrum exhibits an analogous quasi-isotropic range, whose width grows linearly with wall distance. At the present Reynolds numbers, nothing can be said about a possible streamwise similarity, due to limited scale separation. An extensive set of statistics from the simulations is downloadable from ftp://torroja.dmt.upm.es/channels.

537 citations


01 Nov 2003
TL;DR: In this article, the spectra and correlations of the velocity fluctuations in turbulent channels, especially above the buffer layer, were analyzed using direct numerical simulations with friction Reynolds numbers up to Re at very large ones.
Abstract: The spectra and correlations of the velocity fluctuations in turbulent channels, especially above the buffer layer, are analysed using new direct numerical simulations with friction Reynolds numbers up to Re at very large ones.

81 citations


Book ChapterDOI
01 Jan 2003
TL;DR: In this article, the authors studied the large anisotropic scales in turbulent channels, their origin and structure, and their possible influence on other flow properties, including the relation of the different velocity components.
Abstract: It has long been realized that turbulent flows contain a wide range of scales, from small viscous ones responsible for the viscous dissipation, to large ones which carry the turbulent energy and the Reynolds stresses. The former are believed to be roughly universal among different flows, while the latter vary with the geometry and with the flow conditions. Evidence has accumulated for some time that in an intermediate layer of wall-bounded shear flows, including the logarithmic region and part of the outer layer, these large scales are very anisotropic and very large, with streamwise lengths that may be of the order of 100 times their distance to the wall [2,4,8]. At their longest, somewhat above the top of the logarithmic layer, this amounts to 20–30 times the boundary layer thickness. The earliest detailed study of these structures was done by Perry [9,10], who identified them as an E uu ~ k -1, long-wavelength, spectral range. Since the turbulent energy is proportional to ∫ k E uu d (log k), a k -1 spectral range essentially contains most of the fluctuating energy in the flow (see figure 1). Moreover, because the size of these structures requires either very large computational boxes or very long experiments, relatively little was known about them until recently. There is for example very little information on their spanwise dimensions, or on the relation of the different velocity components. The goal of the simulations discussed here is to study the large anisotropic scales in turbulent channels, their origin and structure, and their possible influence on other flow properties.