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Unsteady turbulent plume models

Published online by Cambridge University Press:  12 March 2012

M. M. Scase*
Affiliation:
Faculty of Engineering, University of Nottingham, Nottingham NG7 2RD, UK
R. E. Hewitt
Affiliation:
School of Mathematics, The University of Manchester, Oxford Road, Manchester M13 9PL, UK
*
Email address for correspondence: matthew.scase@nottingham.ac.uk

Abstract

Four existing integral models of unsteady turbulent plumes are revisited. We demonstrate that none of these published models is ideal for general descriptions of unsteady behaviour and put forward a modified model. We show that the most recent (top-hat) plume model (Scase et al. J. Fluid Mech., vol. 563, 2006, p. 443), and the earlier (Gaussian) plume models (Delichatsios J. Fluid Mech., vol. 93, 1979, p. 241; Yu Trans. ASME, vol. 112, 1990, p.186), are all ill-posed. This ill-posedness arises from the downstream growth of short-scale waves, which have an unbounded downstream growth rate. We show that both the top-hat and the Gaussian (Yu) models can be regularized, rendering them well-posed, by the inclusion of a velocity diffusion term. The effect of including this diffusive mechanism is to include a vertical structure in the model that can be interpreted as representing the vertical extent of an eddy. The effects of this additional mechanism are small for steady applications, and cases where the plume forcing can be considered to follow a power law (both of which have been studied extensively). However, the inclusion of diffusion is shown to be crucial to the general initial-value problem for unsteady models.

Type
Papers
Copyright
Copyright © Cambridge University Press 2012

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References

1. Abramowitz, M. & Stegun,  (Eds) 1965 Handbook of Mathematical Functions with Formulas, Graphs and Mathematical Tables. Dover.Google Scholar
2. Delichatsios, 1979 Time similarity analysis of unsteady buoyant plumes in neutral surroundings. J. Fluid Mech. 93, 241250.CrossRefGoogle Scholar
3. Hewitt, R. E. & Duck, P. W. 2011 Pulsatile jets. J. Fluid Mech. 670, 240259.CrossRefGoogle Scholar
4. Holland, P. R. 2011 Oscillating dense plumes. J. Phys. Oceanogr. 41 (8), 14651483.CrossRefGoogle Scholar
5. Hunt, G. R. & van den Bremer, T. S. 2010 Classical plume theory: 1937–2010 and beyond. IMA J. Appl. Maths 76 (3), 424448.CrossRefGoogle Scholar
6. Jospeh, D. & Saut, J. C. 1990 Short-wave instabilities and ill-posed initial-value problems. Theor. Comput. Fluid Dyn. 1, 191227.Google Scholar
7. Kaminski, E., Tait, S. & Carazzo, G. 2005 Turbulent entrainment in jets with arbitrary buoyancy. J. Fluid Mech. 526, 361376.CrossRefGoogle Scholar
8. Kaye, N. B. 2008 Turbulent plumes in stratified environments: A review of recent work. Atmos.-Ocean 46 (4), 433441.CrossRefGoogle Scholar
9. Morton, B. R., Taylor, G. I. & Turner, J. S. 1956 Buoyant gravitational convection from instantaneous and maintained point sources. Proc. R. Soc. Lond. A 234, 123.Google Scholar
10. Papanicolaou, P. N. & List, E. J. 1988 Investigations of round vertical buoyant jets. J. Fluid Mech. 195, 341391.CrossRefGoogle Scholar
11. Prandtl, L. 1952 The Essentials of Fluid Dynamics. Blackie & Son Ltd.Google Scholar
12. Ricou, F. P. & Spalding, D. B. 1961 Measurements of entrainment by axisymmetric turbulent jets. J. Fluid Mech. 8, 2132.CrossRefGoogle Scholar
13. Rooney, G. G. & Linden, P. F. 1996 Similarity considerations for non-Boussinesq plumes in an unstratified environment. J. Fluid Mech. 318, 237250.CrossRefGoogle Scholar
14. Rouse, H., Yih, C. S. & Humphreys, H. W. 1952 Gravitational convection from a boundary source. Tellus 4, 201210.Google Scholar
15. Scase, M. M. 2009 Evolution of volcanic eruption columns. J. Geophys. Res. 114, F04003.Google Scholar
16. Scase, M. M., Aspden, A. J. & Caulfield, C. P. 2009 The effect of sudden source buoyancy flux increases on turbulent plumes. J. Fluid Mech. 635, 137169.CrossRefGoogle Scholar
17. Scase, M. M., Caulfield, C. P. & Dalziel, S. B. 2006a Boussinesq plumes with decreasing source strengths in stratified environments. J. Fluid Mech. 563, 463472.CrossRefGoogle Scholar
18. Scase, M. M., Caulfield, C. P. & Dalziel, S. B. 2008 Temporal variation of non-ideal plumes with sudden reductions in buoyancy flux. J. Fluid Mech. 600, 181199.CrossRefGoogle Scholar
19. Scase, M. M., Caulfield, C. P., Dalziel, S. B. & Hunt, J. C. R. 2006b Time-dependent plumes and jets with decreasing source strengths. J. Fluid Mech. 563, 443461.CrossRefGoogle Scholar
20. Scase, M. M., Caulfield, C. P., Linden, P. F. & Dalziel, S. B. 2007 Local implications for self-similar turbulent plume models. J. Fluid Mech. 575, 257265.CrossRefGoogle Scholar
21. Schmidt, F. H. 1957 On the diffusion of heated jets. Tellus 9, 378383.CrossRefGoogle Scholar
22. Schmidt, W. 1941 Turbulente Ausbreitung eines Stromes erhitzter Luft. Z. Angew. Math. Mech. 21 (6), 351363.CrossRefGoogle Scholar
23. Turner, J. S. 1962 The ‘starting plume’ in neutral surroundings. J. Fluid Mech. 13, 356368.CrossRefGoogle Scholar
24. Vul’fson, A. N. 2001a Convective-region top front propagation in a uniform medium under the action of point, linear, and plane heat and momentum sources. Fluid Dyn. 36 (3), 418428 (translation from Izv. Ross. Acad. Nauk, Mekh. Zhid. i Gaza (3), 90–101).CrossRefGoogle Scholar
25. Vul’fson, A. N. 2001b Unsteady self-similar convection from a point source of heat and passive tracer in a neutral atmosphere. Russ. Met. Hyd. 1, 2335.Google Scholar
26. Vul’fson, A. N. & Borodin, O. O. 2001 Self- similar propagation regimes of a non stationary high temperature convective jet in the adiabatic atmosphere. J. Appl. Mech. Tech. Phys. 42 (2), 255261.CrossRefGoogle Scholar
27. Yu, H.-Z. 1990 Transient plume influence in measurement of convective heat release rates of fast-growing fires using a large-scale fire products collector. Trans. ASME 112, 186191.CrossRefGoogle Scholar