A two-dimensional numerical model for a turbidity current

被引:31
作者
Felix, M [1 ]
机构
[1] Univ Leeds, Sch Earth Sci, Leeds, W Yorkshire, England
来源
PARTICULATE GRAVITY CURRENTS | 2001年 / 31期
关键词
D O I
10.1002/9781444304275.ch5
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
A 2-D numerical model for flow of and deposition from a turbidity current was developed to simulate processes on a natural scale and topography for flows with sand-size sediment. The velocity of the bulk fluid (sediment + water) is calculated from a momentum equation that is derived from the Navier-Stokes equation using the hydrostatic and boundary layer approximations. Sediment concentrations are calculated with advection-diffusion equations for each grain size and turbulence is taken into account by using the Mellor-Yamada level 21/2 second-order closure model. The effect of the presence of particles on the turbulence other than through buoyancy is incorporated through a drag term that leads to an extra dissipation term in the turbulent kinetic energy equation and in the turbulent lengthscale equation. The equations are solved numerically using a finite volume method on a non-staggered grid with a BDF method. Model results are shown for two flows with different initial concentrations. showing the behaviour of the model.
引用
收藏
页码:71 / 81
页数:11
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