Technical Papers
Dec 7, 2012

Gravity Currents Propagating on Sloping Boundaries

Publication: Journal of Hydraulic Engineering
Volume 139, Issue 6

Abstract

Three-dimensional direct numerical simulations of gravity currents on different bottom slopes are presented in this paper. After the buoyancy closed in a lock is instantaneously released, the produced gravity currents go through an acceleration phase followed by a deceleration phase. In the acceleration phase, the tail current connects to and feeds buoyancy into the head for all cases considered here. The maximum buoyancy contained in the head, reached at the end of the acceleration phase, increases as the bottom slope increases. The maximum buoyancy in the head never reaches the total released buoyancy, and a significant portion of released heavy fluid is left in the tail current. In the deceleration phase, the tail current continues to join the head as the gravity currents propagate for lower slope angles (θ=0.2, and 4°), but the head disconnects the joining tail current for higher slope angles (θ=6, 8, and 10°). The gravity current head loses contained buoyancy less rapidly in the deceleration phase as the bottom slope increases. Structures of the gravity current indicate that the relative length of the head diminishes as the gravity currents propagate downslope for lower slope angles and remains approximately constant for higher slope angles. The maximum front velocity increases as the bottom slope increases. In the deceleration phase, the front location–time relationship follows the thermal theory power law for higher slope angles and for lower slope angles, and the inertial phase power-law asymptote is observed.

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Acknowledgments

The author wishes to thank Professor S. Balachandar at the University of Florida for valuable comments at different stages of the work. Computations reported in the study were performed at the National Center for High-Performance Computing in Taiwan. The research was funded by the National Science Council of Taiwan through Projects NSC 98-2218-E-032-007 and NSC 101-2628-E-032-003-MY3. Thanks are also extended to the reviewers for making suggestions that improved the quality of the paper.

References

Allen, J. (1985). Principles of physical sedimentology, Allen & Unwin, London.
Batchelor, G. K. (1967). An introduction to fluid dynamics, Cambridge University Press, Cambridge, UK.
Beghin, P., Hopfinger, E. J., and Britter, R. E. (1981). “Gravitational convection from instantaneous sources on inclined boundaries.” J. Fluid Mech., 107, 407–422.
Birman, V. K., Battandier, B. A., Meiburg, E., and Linden, P. F. (2007). “Lock-exchange flows in sloping channels.” J. Fluid Mech., 577, 53–77.
Birman, V. K., Martin, J. E., and Meiburg, E. (2005). “The non-boussinesq lock-exchange problem. Part 2. High-resolution simulations.” J. Fluid Mech., 537, 125–144.
Bonometti, T., and Balachandar, S. (2008). “Effect of schmidt number on the structure and propagation of density currents.” Theor. Comput. Fluid Dyn., 22(5), 341–361.
Britter, R. E., and Linden, P. F. (1980). “The motion of the front of a gravity current travelling down an incline.” J. Fluid Mech., 99, 531–543.
Cantero, M., Balachandar, S., Garcia, M., and Ferry, J. (2006). “Direct numerical simulations of planar and cylindrical density currents.” J. Appl. Mech., 73(6), 923–930.
Cantero, M., Lee, J., Balachandar, S., and Garcia, M. (2007). “On the front velocity of gravity currents.” J. Fluid Mech., 586, 1–39.
Canuto, C., Hussaini, M., Quarteroni, A., and Zang, T. (1988). Spectral methods in fluid dynamics, Springer, Berlin.
Cortese, T., and Balachandar, S. (1995). “High performance spectral simulation of turbulent flows in massively parallel machines with distributed memory.” Int. J. Supercomput. Appl., 9(3), 187–204.
Dai, A. (2010). “Note on the generalized thermal theory for gravity currents in the deceleration phase.” Dyn. Atmos. Oceans, 50(3), 424–431.
Dai, A., Ozdemir, C. E., Cantero, M. I., and Balachandar, S. (2012). “Gravity currents from instantaneous sources down a slope.” J. Hydraul. Eng., 138(3), 237–246.
Durran, D. (1999). Numerical methods for wave equations in geophysical fluid dynamics, Springer, Berlin.
Ellison, T. H., and Turner, J. S. (1959). “Turbulent entrainment in stratified flows.” J. Fluid Mech., 6, 423–448.
Fannelop, T. K. (1994). Fluid mechanics for industrial safety and environmental protection, Elsevier, Amsterdam, The Netherlands.
Hartel, C., Meiburg, E., and Necker, F. (2000). “Analysis and direct numerical simulation of the flow at a gravity-current head. I: Flow topology and front speed for slip and no-slip boundaries.” J. Fluid Mech., 418, 189–212.
Hopfinger, E. J., and Tochon-Danguy, J. C. (1977). “A model study of powder-snow avalanches.” J. Glaciol., 19(81), 343–356.
Huppert, H., and Simpson, J. (1980). “The slumping of gravity currents.” J. Fluid Mech., 99, 785–799.
La Rocca, M., Adduce, C., Sciortino, G., and Pinzon, A. B. (2008). “Experimental and numerical simulation of three-dimensional gravity currents on smooth and rough bottom.” Phys. Fluids, 20(10), 106603.
Marino, B., Thomas, L., and Linden, P. (2005). “The front condition for gravity currents.” J. Fluid Mech., 536, 49–78.
Maxworthy, T. (2010). “Experiments on gravity currents propagating down slopes. II: The evolution of a fixed volume of fluid released from closed locks into a long, open channel.” J. Fluid Mech., 647, 27–51.
Maxworthy, T., and Nokes, R. I. (2007). “Experiments on gravity currents propagating down slopes. I: The release of a fixed volume of heavy fluid from an enclosed lock into an open channel.” J. Fluid Mech., 584, 433–453.
Morton, B. R., Taylor, G. I., and Turner, J. S. (1956). “Turbulent gravitational convection from maintained and instantaneous sources.” Proc. R. Soc. A, 234, 1–23.
Rastello, M., and Hopfinger, E. J. (2004). “Sediment-entraining suspension clouds: A model of powder-snow avalanches.” J. Fluid Mech., 509, 181–206.
Shin, J., Dalziel, S., and Linden, P. (2004). “Gravity currents produced by lock exchange.” J. Fluid Mech., 521, 1–34.
Simpson, J. (1997). Gravity currents, 2nd Ed., Cambridge University Press, Cambridge, UK.
Williamson, J. H. (1980). “Low-storage Runge-Kutta schemes.” J. Comput. Phys., 35, 48–56.

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Go to Journal of Hydraulic Engineering
Journal of Hydraulic Engineering
Volume 139Issue 6June 2013
Pages: 593 - 601

History

Received: Apr 8, 2012
Accepted: Dec 5, 2012
Published online: Dec 7, 2012
Published in print: Jun 1, 2013

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Dept. of Water Resources and Environmental Engineering, Tamkang Univ., New Taipei City 25137, Taiwan. E-mail: [email protected]

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