NUMERICAL SIMULATION OF LAKE WATER DOWNSTREAM FLOODING DUE TO SUDDEN BREAKAGE OF YIGONG LANDSLIDE DAM IN TIBET
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Graphical Abstract
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Abstract
The dam of the landslide debris barrier lake mainly consists of boulder and stony soil and it is more vulnerable to instability as the result of a rise in water level. The dambreak may cause huge economic property and life loss. Therefore the study of dambreak problem has important academic significance and application value. A highspeed giant landslide occurred in Yigong River in the Bomi,Tibet,on April 9, 2〖CS%0,0,0,0〗〖CS〗000.A landslide dam was formed suddenly with 2500 m long, 2500 m wide and 60 m high, 280~300 million m3 in volume. A debris barrier lake was formed. Taking the dambreak of Yigong barrier lake as an example,according to the continuity equation and NavierStokes equation,combining with standard turbulence model,and tracking the freesurface with VOF method,via computational fluid dynamics software Fluent,this paper analyzes the dambreak flood evolution in downstream river course and the velocity changes at different sites. The simulation results are consistent with the observed data. At the same time,it shows that the model can simply simulate the flood evolution in the river bend with complex terrain after dambreak. The study can provide the prevention of dambreak disaster in terms of downstream flooding.
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