Estimating the integral length scale on turbulent flows from the zero crossings of the longitudinal velocity fluctuation
Autor: | Martin Obligado, Daniel Odens Mora |
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Přispěvatelé: | Laboratoire des Écoulements Géophysiques et Industriels [Grenoble] (LEGI), Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ), Université Grenoble Alpes (UGA) |
Rok vydání: | 2020 |
Předmět: |
Fluid Flow and Transfer Processes
Physics Field (physics) Scale (ratio) Turbulence Autocorrelation Mathematical analysis Computational Mechanics Zero (complex analysis) Fluid Dynamics (physics.flu-dyn) General Physics and Astronomy FOS: Physical sciences Physics - Fluid Dynamics 01 natural sciences Measure (mathematics) 010305 fluids & plasmas [SPI.MECA.MEFL]Engineering Sciences [physics]/Mechanics [physics.med-ph]/Fluids mechanics [physics.class-ph] 010309 optics Mechanics of Materials 0103 physical sciences Calibration ComputingMilieux_MISCELLANEOUS Wind tunnel |
Zdroj: | Experiments in Fluids Experiments in Fluids, Springer Verlag (Germany), 2020, 61 (9), ⟨10.1007/s00348-020-03033-2⟩ |
ISSN: | 0723-4864 1432-1114 |
DOI: | 10.48550/arxiv.2005.06055 |
Popis: | The integral length scale ( $$\mathcal {L}$$ ) is considered to be characteristic of the largest motions of a turbulent flow, and as such, it is an input parameter in modern and classical approaches of turbulence theory and numerical simulations. Its experimental estimation, however, could be difficult in certain conditions, for instance, when the experimental calibration required to measure $$\mathcal {L}$$ is hard to achieve (hot-wire anemometry on large scale wind-tunnels, and field measurements), or in ‘standard’ facilities using active grids due to the behaviour of their velocity autocorrelation function $$\rho (r)$$ , which does not in general cross zero. In this work, we provide two alternative methods to estimate $$\mathcal {L}$$ using the variance of the distance between successive zero crossings of the streamwise velocity fluctuations, thereby reducing the uncertainty of estimating $$\mathcal {L}$$ under similar experimental conditions. These methods are applicable to a variety of situations such as active grids flows, field measurements, and large-scale wind tunnels. |
Databáze: | OpenAIRE |
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