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contributor authorWilliam K. George
contributor authorLuciano Castillo
date accessioned2017-05-08T23:52:13Z
date available2017-05-08T23:52:13Z
date copyrightDecember, 1997
date issued1997
identifier issn0003-6900
identifier otherAMREAD-25742#689_1.pdf
identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/118020
description abstractOf the many aspects of the long-studied field of turbulence, the zero-pressure-gradient boundary layer is probably the most investigated, and perhaps also the most reviewed. Turbulence is a fluid-dynamical phenomenon for which the dynamical equations are generally believed to be the Navier-Stokes equations, at least for a single-phase, Newtonian fluid. Despite this fact, these governing equations have been used in only the most cursory manner in the development of theories for the boundary layer, or in the validation of experimental data-bases. This article uses the Reynolds-averaged Navier-Stokes equations as the primary tool for evaluating theories and experiments for the zero-pressure-gradient turbulent boundary layer. Both classical and new theoretical ideas are reviewed, and most are found wanting. The experimental data as well is shown to have been contaminated by too much effort to confirm the classical theory and too little regard for the governing equations. Theoretical concepts and experiments are identified, however, which are consistent-both with each other and with the governing equations. This article has 77 references.
publisherThe American Society of Mechanical Engineers (ASME)
titleZero-Pressure-Gradient Turbulent Boundary Layer
typeJournal Paper
journal volume50
journal issue12
journal titleApplied Mechanics Reviews
identifier doi10.1115/1.3101858
journal fristpage689
journal lastpage729
identifier eissn0003-6900
keywordsPressure
keywordsBoundary layer turbulence
keywordsGradients
keywordsEquations
keywordsFluids
keywordsTurbulence
keywordsNavier-Stokes equations
keywordsBoundary layers AND Databases
treeApplied Mechanics Reviews:;1997:;volume( 050 ):;issue: 012
contenttypeFulltext


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