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A wind tunnel study of dense gas dispersion in a stable boundary layer over a rough surface

A wind tunnel study of dense gas dispersion in a stable boundary layer over a rough surface
A wind tunnel study of dense gas dispersion in a stable boundary layer over a rough surface
Measurements of the vertical entrainment velocity into two-dimensional dense gas plumes over fully rough surfaces were carried out as part of a co-operative research programme with wind tunnel facilities in the USA. This paper presents results obtained for stable boundary layer conditions in the EnFlo wind tunnel at the University of Surrey; a companion paper treats the neutral boundary layer case. Mean velocity and temperature, turbulent normal and shear tresses, temperature fluctuations and heat fluxes were measured and used to demonstrate that a moderately stable atmospheric boundary layer had been successfully simulated in the tunnel. Entrainment velocities, WE, were then deduced from the streamwise development of the concentration field, non-dimensionalised with respect to the friction velocity in the undisturbed flow, u*, and correlated with the plume Richardson number, Ri*. Higher non-dimensional entrainment speeds, WE/u*, were observed for Ri*>5 in the stable boundary layer than in the neutral boundary layer, the difference growing with increasing Richardson number. Emission velocity ratios, W0/u*, were however larger in the stable experiments, and exceeded one at about Ri*=18. Entrainment in the stable boundary layer appeared therefore to be more sensitive to emission velocity ratio than in the neutral case. Entrainment behaviour for Ri*?5 followed that found in the neutral boundary layer. In this regime, use of the neutral boundary layer entrainment speed correlation is unlikely to lead to the over-prediction of plume dilution rates in moderately stable boundary layers.
entrainment, richardson number, plume depth, plume spread, concentration, lda
1352-2310
2253-2263
Robins, Alan
fae9b9ac-6c19-4f4a-b265-a26cdd675585
Castro, Ian
66e6330d-d93a-439a-a69b-e061e660de61
Hayden, Paul
b5662acc-6375-4f86-afee-04c779155d5f
Steggel, Nathan
1b2d01e6-247c-4fd6-a019-67236355b798
Contini, Daniel
c6ab0a89-e713-41d2-974d-7faa181a58a8
Heist, David
1e935b77-67ce-4782-8b30-2bd251f739b9
Taylor, T. John
5d080558-649a-448f-b2a8-6313c466326d
Robins, Alan
fae9b9ac-6c19-4f4a-b265-a26cdd675585
Castro, Ian
66e6330d-d93a-439a-a69b-e061e660de61
Hayden, Paul
b5662acc-6375-4f86-afee-04c779155d5f
Steggel, Nathan
1b2d01e6-247c-4fd6-a019-67236355b798
Contini, Daniel
c6ab0a89-e713-41d2-974d-7faa181a58a8
Heist, David
1e935b77-67ce-4782-8b30-2bd251f739b9
Taylor, T. John
5d080558-649a-448f-b2a8-6313c466326d

Robins, Alan, Castro, Ian, Hayden, Paul, Steggel, Nathan, Contini, Daniel, Heist, David and Taylor, T. John (2001) A wind tunnel study of dense gas dispersion in a stable boundary layer over a rough surface. Atmospheric Environment, 35 (13), 2253-2263. (doi:10.1016/S1352-2310(01)00073-5).

Record type: Article

Abstract

Measurements of the vertical entrainment velocity into two-dimensional dense gas plumes over fully rough surfaces were carried out as part of a co-operative research programme with wind tunnel facilities in the USA. This paper presents results obtained for stable boundary layer conditions in the EnFlo wind tunnel at the University of Surrey; a companion paper treats the neutral boundary layer case. Mean velocity and temperature, turbulent normal and shear tresses, temperature fluctuations and heat fluxes were measured and used to demonstrate that a moderately stable atmospheric boundary layer had been successfully simulated in the tunnel. Entrainment velocities, WE, were then deduced from the streamwise development of the concentration field, non-dimensionalised with respect to the friction velocity in the undisturbed flow, u*, and correlated with the plume Richardson number, Ri*. Higher non-dimensional entrainment speeds, WE/u*, were observed for Ri*>5 in the stable boundary layer than in the neutral boundary layer, the difference growing with increasing Richardson number. Emission velocity ratios, W0/u*, were however larger in the stable experiments, and exceeded one at about Ri*=18. Entrainment in the stable boundary layer appeared therefore to be more sensitive to emission velocity ratio than in the neutral case. Entrainment behaviour for Ri*?5 followed that found in the neutral boundary layer. In this regime, use of the neutral boundary layer entrainment speed correlation is unlikely to lead to the over-prediction of plume dilution rates in moderately stable boundary layers.

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More information

Published date: 2001
Keywords: entrainment, richardson number, plume depth, plume spread, concentration, lda

Identifiers

Local EPrints ID: 46267
URI: http://eprints.soton.ac.uk/id/eprint/46267
ISSN: 1352-2310
PURE UUID: a3ef0d8a-ec73-4618-84eb-6b3d10856e14

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Date deposited: 11 Jun 2007
Last modified: 15 Mar 2024 09:20

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Contributors

Author: Alan Robins
Author: Ian Castro
Author: Paul Hayden
Author: Nathan Steggel
Author: Daniel Contini
Author: David Heist
Author: T. John Taylor

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