This study describes a two-dimensional numerical model simulating flushing
of sediments from water reservoirs. The numerical model solves the depth-av
eraged Navier-Stokes equations on a two-dimensional grid. A zero-equation t
urbulence model is used. The resulting flow field is extrapolated to three
dimensions, and the convection-diffusion equation for the sediment concentr
ation is solved A formula for the bed concentration is used as boundary con
dition, resulting in a calculation of bed material load. Continuity for the
cells closest to the bed is used to find the bed changes. The pressure fie
ld is used to calculate the location of the water surface. The grid is adap
tive in the vertical;direction, and changes according to the calculated wat
er and bed levels. A porosity model is used to simulate the process when th
e water surface drops under the bed level at some locations of the geometry
. The results: from the numerical model were compared with data from physic
al model studies. The main features of the erosion pattern were reproduced,
and the deviation between the calculated and measured scour volume was sma
ll. This showed that most of the simplifications made in the numerical mode
l were reasonable. There were deviations between measured and calculated be
d levels in a bend. This was most likely due to secondary currents that wer
e not possible to model using a two-dimensional approach.