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On the entrainment assumption in Schatzmann’s integral plume model

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Abstract

The behaviour of stationary, non-passive plumes can be simulated in a reasonably simple and accurate way by integral models. One of the key requirements of these models, but also one of their less well-founded aspects, is the entrainment assumption, which parameterizes turbulent mixing between the plume and the environment. The entrainment assumption developed by Schatzmann and adjusted to a set of experimental results requires four constants and an ad hoc hypothesis to eliminate undesirable terms. With this assumption, Schatzmann’s model exhibits numerical instability for certain cases of plumes with small velocity excesses, due to very fast radius growth. The purpose of this paper is to present an alternative entrainment assumption based on a first-order turbulence closure, which only requires two adjustable constants and seems to solve this problem. The asymptotic behaviour of the new formulation is studied and compared to previous ones. The validation tests presented by Schatzmann are repeated and it is found that the new formulation not only eliminates numerical instability but also predicts more plausible growth rates for jets in co-flowing streams.

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References

  1. Briggs, G.A., Plume rise and buoyancy effects. In: D. Randerson (ed.),Atmospheric Science and Power Production, U.S. Dept. of Energy DOE/TIC-27601 (1984) pp. 327–366.

  2. Chu, V.H. and Goldberg, M.B., Buoyant forced-plumes in cross-flow.J. Hydraulics Division of the ASCE 100 (1974) 10805–10808.

    Google Scholar 

  3. Csanady, G.T.,Turbulent Diffusion in the Environment, Geophysics and Astrophysics Monographs, D. Reidel Publishing Company, Dordrecht (1973) 248 pp.

    Google Scholar 

  4. Davidson, G.A., A discussion of Schatzmann’s integral plume model from a control volume viewpoint.J. Climate Appl. Meteorol. 25 (1986) 858–867.

    Article  ADS  Google Scholar 

  5. Fan, L.N., Turbulent buoyant jets into stratified or flowing ambient fluids. California Institute of Technology, Report No. KH-R-15, Pasadena, CA (1967).

  6. Fink, L., Der axialsymmetrische Strahl in einer turbulenten Grundströmung. SFB 80, Universität Karlsruhe, Report No. SFB 80/ET/20 (1974).

  7. Fox, D.G., Forced plume in a stratified fluid.J. Geophys. Res. 75 (1970) 6818–6835.

    ADS  Google Scholar 

  8. Hirst, E., Buoyant jets discharged to quiescent stratified ambients.J. Geophys. Res. 76 (1971) 7375–7384.

    Article  ADS  Google Scholar 

  9. Hirst, E., Buoyant jets with tree-dimensional trajectories.J. Hydraulics Division of the ASCE 98 (1972) 1999–2014.

    Google Scholar 

  10. Hoult, D.P., Fay, J.A. and Forney, L.J., A theory of plume rise compared with field observations.J. Air Pollut. Control Ass. 19 (1969) 585–590.

    Google Scholar 

  11. Middleton, J.H., The rise of forced plumes in a stably stratified crossflow.Boundary-Layer Meteorol. 36 (1986) 137–199.

    Article  ADS  Google Scholar 

  12. Morton, B.R., Forced plumes.J. Fluid Mech. 5 (1959) 151–163.

    Article  ADS  MathSciNet  MATH  Google Scholar 

  13. Morton, B.R., Taylor, G.I. and Turner, J.S., Turbulent gravitational convection from maintained and instantaneous sources.Proc. Roy. Soc. London A234 (1956) 1–23.

    Article  ADS  MathSciNet  MATH  Google Scholar 

  14. Moussa, Z.M., Trischka, J.W. and Eskinazi, S., The near field in the mixing of a round jet with cross-stream.J. Fluid Mech. 80 (1977) 49–80.

    Article  ADS  Google Scholar 

  15. Priestley, C.H.D., A working theory of the bent-over plume of hot gas.Quart. J. Roy. Met. Soc. 82 (1956) 165–176.

    ADS  Google Scholar 

  16. Priestley, C.H.D. and Ball, F.K., Continuous convection from an isolated source of heat.Quart. J. Roy. Meteorol. Soc. 81 (1955) 144–157.

    ADS  Google Scholar 

  17. Schatzmann, M., The integral equations for round buoyant jets in stratified flows.J. Appl. Math. Phys. (ZAMP) 29 (1978) 608–630.

    Article  MathSciNet  MATH  Google Scholar 

  18. Schatzmann, M., An integral model of plume rise.Atmos. Environ. 13 (1979) 721–731.

    Article  Google Scholar 

  19. Schatzmann, M. and Policastro, A.J., Effects of the Boussinesq approximation on the results of strongly buoyant plume calculations.J. Climate Appl. Meteorol. 23 (1984) 117–123.

    Article  ADS  Google Scholar 

  20. Slawson, P.R. and Csanady, G.T., On the mean path of buoyant, bent-over chimney plumes.J. Fluid Mech. 28 (1967) 311–322.

    Article  ADS  Google Scholar 

  21. Slawson, P.R. and Csanady, G.T., The effect of atmospheric conditions on plume rise.J. Fluid Mech. 47 (1979) 39–49.

    Google Scholar 

  22. Weil, J.C., Plume rise. In: Venkatram, A. and Wyngaard, J.C. (eds),Lectures on Air Pollution Modeling. American Meteorological Society, Boston (1988) pp. 119–162.

    Google Scholar 

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Teixeira, M.A.C., Miranda, P.M.A. On the entrainment assumption in Schatzmann’s integral plume model. Appl. Sci. Res. 57, 15–42 (1996). https://doi.org/10.1007/BF02528762

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  • DOI: https://doi.org/10.1007/BF02528762

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