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Exploratory temperature-tagging measurements of turbulent spots in a heated laminar boundary layer

Published online by Cambridge University Press:  19 April 2006

C. W. Van Atta
Affiliation:
Institute for Pure and Applied Physical Sciences and Department of Applied Mechanics and Engineering Sciences, University of California, San Diego, La Jolla, California 92093
K. N. Helland
Affiliation:
Institute for Pure and Applied Physical Sciences and Department of Applied Mechanics and Engineering Sciences, University of California, San Diego, La Jolla, California 92093

Abstract

Exploratory measurements to study transport mechanisms in turbulent spots have been made using a passive temperature-tagging technique. Temperature fluctuations were measured on the centre-plane of spots artificially generated in the laminar boundary layer on a fully heated flat plate. The fluid near the wall is cooled and fluid far from the wall is heated during passage of the spot, with a more complex behaviour at intermediate locations. Contours of ensemble-averaged temperature disturbance measured relative to the laminar undisturbed profile show a region of maximum heating near the upper front of the spot and a region of maximum cooling at the rear of the spot near the wall, a structure strongly anti-correlated with corresponding contours of the longitudinal velocity disturbance as measured by Zilberman, Wygnanski & Kaplan (1977). The observed position of the upper heating maximum appears to be related to mean streamline pictures obtained by previous investigators in which streamlines entering the rear of the spot are deflected upward into the heated region. In conical similarity co-ordinates there is a near coincidence of the maxima and minima in the temperature disturbance contours with the two stable foci, or points of accumulation, for particle paths found by Cantwell, Coles & Dimotakis (1978), but the position of the hot core region cannot be explained in terms of the centre-line particle paths. An alternate viscosity-dependent scaling produces closer coincidence of the temperature and velocity disturbance extrema with the foci.

Type
Research Article
Copyright
© 1980 Cambridge University Press

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