Martín Bautista, Juan A. and Martel Escobar, Carlos (2008) Streaky 3D Structures in the Boundary Layer. In: 61st Annual Meeting of Division of Fluid Dynamics, 23/11/2008-25/11/2008, San Antonio, TEXAS (EEUU).
Ver estadisticas de descargas para este eprint (solo desde ordenadores de la UPM)| Item Type: | Presentation at Congress or Day (Poster) | ||||||
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| Title: | Streaky 3D Structures in the Boundary Layer | ||||||
| Event Title: | 61st Annual Meeting of Division of Fluid Dynamics | ||||||
| Event Dates: | 23/11/2008-25/11/2008 | ||||||
| Event Location: | San Antonio, TEXAS (EEUU) | ||||||
| Title of Book: | Posters of 61st Annual Meeting of Division of Fluid Dynamics | ||||||
| Date: | 2008 | ||||||
| Department: | Mathematical Fundamentals of Aeronautics Technology | ||||||
| Faculty: | E.T.S.I. Aeronautical (UPM) | ||||||
| Creative Commons licenses: | Recognition - No derivative works - No commercial | ||||||
| Item ID: | 3292 | ||||||
| Subjects: | Mathematics Aeronautics |
Texto completo disponible como:
| PDF 1132Kb - Idioma: English |
Official URL: http://dfd2008.tamu.edu/index.html
Abstract
It has been recently shown [Choi, Nature, April 06 - Cossu, PRL, February 06] that 3D streaky structures in the boundary layer can remain laminar longer than the 2D Blasius °ow. The aim of this investigation is to study the possibility of promoting these 3D streaky structures via surface roughness, computing them and evaluat- ing the resulting stabilization using the Reduced Navier Stokes equations (RNS). The RNS are derived from Navier-Stokes making use of the fact that two very di®erent scales are present: one slow (streamwise direc- tion) and two short (spanwise and wall-normal direction). The RNS allows us to perform these 3D computations in a standard PC, without using CPU costly DNS simulations.
| Item Type: | Presentation at Congress or Day (Poster) |
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| Subjects: | Mathematics Aeronautics |
| Código ID: | 3292 |
| Depositado Por: | Memoria Investigacion |
| Depositado el: | 11 Jun 2010 10:37 |
| Last Modified: | 11 Jun 2010 14:10 |
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