Abstract
The effect of entrainment and the role of the interface during the interaction between an axisymmetric turbulent mass plume and a strong stratified layer are investigated. We describe mainly the characteristics of the plume: the change in the profiles of the density, the horizontal component of the velocity and the corresponding intensity of turbulence, the change in the entrainment co-efficient, when the plume goes through the impingement interface, assuming a self-similar Gaussian property of the axial velocity component and of the density difference. The influence of the stratification on the plume angle coefficient is studied, and compared with the results related to a homogeneous environment, obtained elsewhere. Experimental correlation on the mean entrainment coefficient in a given plume cross-section, is formulated.
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Abbreviations
- B :
-
specific buoyancy flux at the source \(( = {\text{g}}Q{\text{ }}(\rho _{air} - \rho _{He} )/\rho _{He} )\)
- d :
-
diameter of the source
- Fr :
-
Froude number = \({\text{U}}_{\text{0}}^{\text{2}} \rho _{He} {\text{/gd}}(\rho _{air} - \rho _{He} )\) (at the source)
- g :
-
magnitude of gravitational acceleration
- I :
-
turbulence intensity
- K :
-
coefficient in relation with the entrainment
- l m :
-
characteristic length (= M 0.750 B −0.5)
- m :
-
mass flow rate
- M :
-
momentum flux
- M 0 :
-
specific momentum flux at the source (=QU 0)
- N :
-
Brunt-Väisälä frequency \(\left( {N^2 = \left\{ {\frac{{ - g{\text{ }}d\rho _\infty }}{{\rho _{air} {\text{ }}d{\text{x}}}}} \right\}} \right)\)
- N * :
-
dimensionless N (N *=N(l m/g)0.5)
- Q :
-
volumetric flow rate (at the source = U 0 S)
- r :
-
radial coordinate
- r 1 :
-
radial coordinate at the point where \(\bar u/\bar u_c = \frac{1}{e}\)
- r sup′inf1 :
-
radial coordinate at the point where \(\Delta \bar \rho /\Delta \bar \rho c = \frac{1}{e}\)
- Re :
-
Reynolds number (at the source \(\operatorname{Re} _0 = U_0 d/v_{He} \))
- Ri :
-
Richardson number (at the source Ri 0 = Fr1/2)
- u :
-
vertical velocity component
- U :
-
vertical mean velocity
- v :
-
radial velocity component
- x :
-
vertical coordinate distance
- x v :
-
virtual origin of the plume
- \(\hat x = \frac{x}{d}\) :
-
dimensionless vertical coordinate distance
- X * :
-
dimensionless parametric group, defined in (Eq. (17))
- α :
-
entrainment coefficient
- ϱ :
-
fluid density
- \(\Delta \rho = \rho - \rho _\infty \) :
-
density difference
- \(\hat \tau = \frac{{\rho - \rho _{air} }}{{\rho _{He} - \rho _{air} }}\) :
-
dimensionless density
- air:
-
air
- c :
-
on the axis of the flow
- He:
-
helium
- m :
-
relative to minimum value or maximum value
- 0:
-
value at the source
- v :
-
corresponding to the radial velocity
- ∞:
-
ambient conditions
- ∧:
-
dimensionless value
- −:
-
mean value
- ':
-
fluctuation
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Dehmani, L., Son, D.K., Gbahoué, L. et al. Influence of a strong density stratification on the entrainment of a turbulent axisymmetric plume. Experiments in Fluids 21, 170–180 (1996). https://doi.org/10.1007/BF00191688
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DOI: https://doi.org/10.1007/BF00191688