| Seminar Announcement |
Gravity Currents Propagating Over an Array of
Bottom Obstacles
George Contantinescu
Associate Professor
Department of Civil and Environmental Engineering
IIHR-Hydroscience and Engineering
University of Iowa
Iowa City, IA 52242
Highly resolved 3-D Large Eddy Simulation (LES) is used to study the
interaction between a lock-exchange gravity current with a large
volume of release and an array of bottom-mounted large-scale obstacles
in the form of 2-D dunes or square ribs. The study of the interaction
between a gravity current and an array of obstacles is important for
many practical applications. For example, arrays of obstacles are
often used as protective measures on the hilly terrains and on the
skirts of the mountains to stop or slow down gravity currents in the
form of powder-snow avalanches. Even if they do not arrest the flow,
the retarding obstacles reduce the impact of the avalanche with the
buildings situated downstream of the obstacles. The temporal variation
of the impact forces on the obstacles is analyzed. This information is
needed for the design of the retarding obstacles. Additionally,
simulation results are used to understanding how this variation is
related to the passage of the backward propagating hydraulic jumps and
the different flow structures that develop within the flow. The loose
bed surface over which the gravity current propagates in the
environment is often not flat. Bed forms, typically in the form of
ripples, dunes or anti-dunes are present at the seafloor or river
bed. The presence of large-scale bedforms provides an additional
mechanism for energy dissipation and can substantially modify the
capacity of a compositional gravity current to entrain sediment with
respect to the case of a flat bed. LES is used to understand how the
shape and the relative size of the large-scale obstacles (roughness
elements) affect the front velocity, the structure of the current, the
energy balance, the bed shear distributions and sediment entrainment
capacity of the current as it propagates over a loose bed. Finally,
scale effects are investigated between Reynolds numbers at which most
of the laboratory studies are conducted (Re~104) and
Reynolds numbers that are within the lower range of those encountered
in the field (Re=106).
Wednesday, November 11, 2009
3:30 PM
Stauffer Science Lecture Hall, Room 100 (SLH 100)
Refreshments will be served at 3:15 pm.
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