A wind tunnel study of dense gas dispersion in a neutral boundary layer over a rough surface
Robins, Alan, Castro, Ian, Hayden, Paul, Steggal, Nathan, Contini, Daniele and Heist, David (2001) A wind tunnel study of dense gas dispersion in a neutral boundary layer over a rough surface. Atmospheric Environment, 35, (13), 2243-2252. (doi:10.1016/S1352-2310(01)00072-3).
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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 neutral boundary layer conditions in the EnFlo wind tunnel at the University of Surrey; a companion paper treats the stable boundary layer case. Entrainment velocities, WE, were 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*. Results for Richardson numbers in the range Ri*<15 were found to be well fitted by the empirical expression: WE/u*=0.65/(1+0.2Ri*). Flow visualisation studies showed layered plume structures with a sharp upper interface at higher Richardson numbers and in this regime turbulent motion below the interface became progressively more intermittent as Ri* increased. Measured turbulence levels collapsed within such high Richardson number plumes and flow and dispersion were significantly affected by molecular processes. Up-welling above the source was observed when the emission speed exceeded the approach flow friction velocity, though there was no clear evidence that this affected plume behaviour away from the immediate vicinity of the source.
|Keywords:||entrainment, Richardson number, plume depth, plume spread, concentration, LDA|
|Subjects:||T Technology > T Technology (General)|
|Divisions:||University Structure - Pre August 2011 > School of Engineering Sciences
|Date Deposited:||15 Mar 2006|
|Last Modified:||06 Aug 2015 02:20|
|RDF:||RDF+N-Triples, RDF+N3, RDF+XML, Browse.|
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