Abstract
IN a paper published in 1884, Prof. Osborne Reynolds1 expressed the opinion that free surfaces, as found in open channels, tend to be “conducive to direct or steady motion”. Thus we should expect the critical Reynolds number for open channels to be, in general, higher than it is for pipes, using the hydraulic radius as the length-parameter throughout.
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References
Reynolds, Osborne, Proc. Roy. Inst., 11, 44 (1884–86).
Stanton, T. E., and Pannell, J. R., Phil. Trans. Roy. Soc., A, 214, 199 (1914).
Davies, S. J., and White, C. M., Proc. Roy. Soc., 119 (1928).
Cornish, R. J., Proc. Roy. Soc., A., 120, 691 (October 1928).
Allen, J., Phil. Mag., Ser. 7, 18, 488 (September 1934).
Allen, J., Phil. Mag. and J. Sci., 7th Ser., 17, 1081 (June 1934).
Horton, R. E., Leach, H. R., and Vliet, R. van, Trans. Amer. Geophys. Union, 1933–34 (graph on p. 402).
Straub, Lorenz G., Trans. Amer. Geophys. Union, Part 4, 649 (August 1939).
Owen, W. M., Trans. Amer. Soc. Civ. Eng., 119, 1165 (1954).
Straub, Lorenz G., Silverman, E., and Nelson, H. C., Trans. Amer. Soc. Civ. Eng., 123, 685 (1958).
Paper 17, U.S. Waterways Exp. Stat., Vicksberg, Mississippi (January 1935).
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ALLEN, J. Laminar and Turbulent Flow in Open Channels. Nature 208, 1196–1197 (1965). https://doi.org/10.1038/2081196a0
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DOI: https://doi.org/10.1038/2081196a0
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