The turbulent Prandtl number in a pure plume is 3/5
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Published version
Accepted version
Author(s)
Craske, J
Salizzoni, P
van Reeuwijk, M
Type
Journal Article
Abstract
We derive a new expression for the entrainment coefficient in a turbulent plume using
an equation for the squared mean buoyancy. Consistency of the resulting expression
with previous relations for the entrainment coefficient implies that the turbulent Prandtl
number in a pure plume is equal to 3
/
5 when the mean profiles of velocity and buoyancy
have a Gaussian form of equal width. Entrainment can be understood in terms of the
volume flux, the production of turbulence kinetic energy or the production of scalar
variance for either active or passive variables. The equivalence of these points of view
indicates how the entrainment coefficient and the turbulent Prandtl and Schmidt numbers
depend on the Richardson number of the flow, the ambient stratification and the relative
widths of the velocity and scalar profiles. The general framework is valid for self-similar
plumes, which are characterised by a power-law scaling. For jets and pure plumes it is
shown that the derived relations are in reasonably good agreement with results from
direct numerical simulations and experiments.
an equation for the squared mean buoyancy. Consistency of the resulting expression
with previous relations for the entrainment coefficient implies that the turbulent Prandtl
number in a pure plume is equal to 3
/
5 when the mean profiles of velocity and buoyancy
have a Gaussian form of equal width. Entrainment can be understood in terms of the
volume flux, the production of turbulence kinetic energy or the production of scalar
variance for either active or passive variables. The equivalence of these points of view
indicates how the entrainment coefficient and the turbulent Prandtl and Schmidt numbers
depend on the Richardson number of the flow, the ambient stratification and the relative
widths of the velocity and scalar profiles. The general framework is valid for self-similar
plumes, which are characterised by a power-law scaling. For jets and pure plumes it is
shown that the derived relations are in reasonably good agreement with results from
direct numerical simulations and experiments.
Date Issued
2017-07-10
Date Acceptance
2017-04-18
Citation
Journal of Fluid Mechanics, 2017, 822, pp.774-790
ISSN
0022-1120
Publisher
Cambridge University Press
Start Page
774
End Page
790
Journal / Book Title
Journal of Fluid Mechanics
Volume
822
Copyright Statement
© 2017 Cambridge University Press
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
Sponsor
EPSRC
Subjects
Science & Technology
Technology
Physical Sciences
Mechanics
Physics, Fluids & Plasmas
Physics
plumes/thermals
stratified turbulence
turbulent mixing
GRAVITATIONAL CONVECTION
BUOYANT PLUME
ROUND JET
ENTRAINMENT
TEMPERATURE
Fluids & Plasmas
01 Mathematical Sciences
09 Engineering
Publication Status
Published
Date Publish Online
2017-06-08