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Temporal variation of non-ideal plumes with sudden reductions in buoyancy flux

Published online by Cambridge University Press:  26 March 2008

M. M. SCASE*
Affiliation:
Department of Applied Mathematics and Theoretical Physics, University of Cambridge, Centre for Mathematical Sciences, Wilberforce Road, Cambridge CB3 0WA, UK
C. P. CAULFIELD
Affiliation:
Department of Applied Mathematics and Theoretical Physics, University of Cambridge, Centre for Mathematical Sciences, Wilberforce Road, Cambridge CB3 0WA, UK BP Institute, University of Cambridge, Madingley Road, Cambridge CB3 0EZ, UK
S. B. DALZIEL
Affiliation:
Department of Applied Mathematics and Theoretical Physics, University of Cambridge, Centre for Mathematical Sciences, Wilberforce Road, Cambridge CB3 0WA, UK

Abstract

We model the behaviour of isolated sources of finite radius and volume flux which experience a sudden drop in buoyancy flux, generalizing the previous theory presented in Scase et al. (J. Fluid Mech., vol. 563, 2006, p. 443). In particular, we consider the problem of the source of an established plume suddenly increasing in area to provide a much wider plume source. Our calculations predict that, while our model remains applicable, the plume never fully pinches off into individual rising thermals.

We report the results of a large number of experiments, which provide an ensemble to compare to theoretical predictions. We find that provided the source conditions are weakened in such a way that the well-known entrainment assumption remains valid, the established plume is not observed to pinch off into individual thermals. Further, not only is pinch-off not observed in the ensemble of experiments, it cannot be observed in any of the individual experiments. We consider both the temporal evolution of the plume profile and a concentration of passive tracer, and show that our model predictions compare well with our experimental observations.

Type
Papers
Copyright
Copyright © Cambridge University Press 2008

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References

REFERENCES

Baines, W. D. & Turner, J. S. 1969 Turbulent and buoyant convection from a source in a confined region. J. Fluid Mech. 37, 5180.Google Scholar
Batchelor, G. K. 1954 Heat convection and buoyancy effects in fluids. Q. J. R. Met. Soc. 80, 339358.CrossRefGoogle Scholar
Carazzo, G., Kaminski, E. & Tait, S. 2006 The route to self-similarity in turbulent jets and plumes. J. Fluid Mech. 547, 137148.CrossRefGoogle Scholar
Caulfield, C. P. 1991 Stratification and buoyancy in geophysical flows. PhD Thesis, University of Cambridge, UK.Google Scholar
Caulfield, C. P. & Woods, A. W. 1995 Plumes with non-monotonic mixing behaviour. Geophys. Astrophys. Fluid Dyn. 79, 173199.Google Scholar
Caulfield, C. P. & Woods, A. W. 1998 Turbulent gravitational convection from a point source in a non-uniformly stratified environment. J. Fluid Mech. 360, 229248.Google Scholar
Dalziel, S. B. 2006 DL Research Partners, http://www.damtp.cam.ac.uk/lab/digiflowGoogle Scholar
Hunt, G. R. & Kaye, N. B. 2001 Virtual origin correction for lazy turbulent plumes. J. Fluid Mech. 435, 377396.Google Scholar
Hunt, G. R. & Linden, P. F. 2001 Steady-state flows in an enclosure ventilated by buoyancy forces assisted by wind. J. Fluid Mech. 426, 355386.Google Scholar
Hunt, J. C. R., Vrieling, A. J., Nieuwstadt, F. T. M. & Fernando, H. J. S. 2003 The influence of the lower boundary on eddy motion in convection. J. Fluid Mech. 491, 183205.Google Scholar
Kaminski, E., Tait, S. & Carazzo, G. 2005 Turbulent entrainment in jets with arbitrary buoyancy. J. Fluid Mech. 526, 361376.Google Scholar
Morton, B. R. 1959 Forced plumes. J. Fluid Mech. 5, 151163.CrossRefGoogle Scholar
Morton, B. R., Taylor, G. I. & Turner, J. S. 1956 Turbulent gravitational convection from maintained and instantaneous sources. Proc. R. Soc. Lond. A 234, 132.Google Scholar
Scase, M. M., Caulfield, C. P. & Dalziel, S. B. 2006 a Boussinesq plumes with decreasing source strengths in stratified environments. J. Fluid Mech. 563, 463472 (herein referred to as S06a.).CrossRefGoogle Scholar
Scase, M. M., Caulfield, C. P., Dalziel, S. B. & Hunt, J. C. R. 2006 b Time-dependent plumes and jets with decreasing source strengths. J. Fluid Mech. 563, 443461 (herein referred to as S06b.).Google Scholar
Scase, M. M., Caulfield, C. P., Dalziel, S. B. & Hunt, J. C. R. 2006 c Plumes and jets with time-dependent sources in stratified and unstratified environments. In Proc. 6th Intl Symp. on Stratified Flows (ed. Ivey, G. N.), 112–117.Google Scholar
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
Wong, A. B. D., Griffiths, R. W. & Hughes, G. O. 2001 Shear layers driven by turbulent plumes. J. Fluid Mech. 434, 209241.CrossRefGoogle Scholar
Woods, A. W. 1997 A note on non-Boussinesq plumes in an incompressible stratified environment. J. Fluid Mech. 345, 347356.CrossRefGoogle Scholar