Estimating Bed-Load Advection And Dispersion Coefficients With The Method Of Moments

被引:0
|
作者
Ramos, Kervi [1 ]
Gibson, Stanford [1 ]
Kavvas, Levent M. [2 ]
Heath, Ronnie [3 ]
Sharp, Jeremy [3 ]
机构
[1] US Army, Corps Engineers, Hydrol Engn Ctr, Inst Water Resources, 609 Second St, Davis, CA 95616 USA
[2] Univ Calif Davis, Dept Civil & Environm Engn, Davis, CA 95616 USA
[3] US Army, Corps Engineers, Engn Res & Dev Ctr, Costal & Hydraul Lab, Vicksburg, MS 39180 USA
来源
WORLD ENVIRONMENTAL AND WATER RESOURCES CONGRESS 2015: FLOODS, DROUGHTS, AND ECOSYSTEMS | 2015年
关键词
TRANSPORT;
D O I
暂无
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The Advection Dispersion (AD) equation is commonly used to simulate solute, wash load, and even suspended load transport, but is rarely applied to bed load. The obstacle to applying AD equation to bed load transport is empirical; it is challenging to estimate the advection and diffusion coefficients. This paper applies the method of moments to a flume experiment to compute the AD bed load coefficients. Five colors of otherwise identical sand were introduced into an equilibrium sediment flume in sequence. After the experiment, surface, bed samples were collected along the length of the flume and sieved into eight-grain classes. Color distributions of each sample and each grain class were computed with image analysis. Longitudinal Probability Mass Function (PMF) of each color and each grain class were computed from these data. The method of moments was applied to the PMF of the particle displacements, where the advection coefficient was the temporal derivative of the first moment of each color and, the diffusion coefficient was defined as the temporal derivative of the variance. In this paper, advection and dispersion coefficients are computed for coarse sand material that consists of mean diameter of 1.3mm
引用
收藏
页码:1736 / 1741
页数:6
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