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Experimental study on average movement characteristics
of bed-load particles |
| Limo TANG1,Xingkui WANG2, |
| 1.State Key Laboratory
of Hydrology-Water Resources and Hydraulic Engineering, Hohai University,
Nanjing 210098, China; 2.State Key Laboratory
of Hydroscience and Engineering, Tsinghua University, Beijing 100084,
China; |
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Abstract The three-dimensional movements of bed-load particles in an open channel with different grain diameters and different specific gravities under the conditions of different hydraulic gradient are measured by means of particle tracking velocimetry (PTV) technique. The average movement characteristics of the particles are analyzed by statistics. The results show that the longitudinal average velocities of the particles neither agree with the law suggested by Einstein nor obey the law assumed by Bagnold. Einstein’s law is that the particle velocity is equal to 11.6 times of shear velocity, and the Bagnold’s law assumes the velocity equal to the difference between flow velocity at corresponding water depth and settling velocity of particle. Two formulas for determining the velocity of particle in the forms of expression given by Einstein and Bagnold are obtained according to the statistical results of experimental data, respectively.
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Issue Date: 05 December 2009
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Einstein H A. The bed load function for sediment transportation in open channelflows. Technical Bulletin/ United StatesDepartment of Agriculture, 1950, 1026: 71
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Tang Limo, Yu Mingzhong, Liu Chunjing, Wang Xingkui. The developmentand elementary application of 3-D partricle tracking velocimetry. Journal of Hydraulic Engineering,??2006, 37(11): 1378―1383 (in Chinese)
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