The movement of oil under non-breaking waves.
The combined effects of wave kinematics, turbulent diffusion, and buoyancy on the transport of oil droplets at sea were investigated in this work using random walk techniques in a Monte Carlo framework. Six hundred oil particles were placed at the water surface and tracked for 500 wave periods. A dimensionless formulation was presented that allowed reporting distances in terms of the wave length and times in terms of the wave period. Stokes' drift was, expectedly, the major mechanism for horizontal transport. It was also found that plumes that have large terminal rise velocities move faster forward but spread less than those that have small terminal rise velocities. The increase in wave slope (or wave steepness) caused an increase in transport and spreading of the plume. Our results supported treating the oil as completely mixed vertically in a layer near the surface. In the horizontal direction, buoyant plumes had spreading coefficients that are essentially constant after about 200 wave periods. But neutrally buoyant plumes had horizontal spreading coefficients that increased with time (for the simulation time of 500 wave periods). Techniques for generalizing the results for a wide range of wave parameters were presented.
Temple University, Department of Civil and Environmental Engineering, 1947 N 12th Street, Philadelphia, PA 19122, USA. boufadel@temple.edu
Michel C
MC
Boufadel
Ryan Daniel
RD
Bechtel
James
J
Weaver
D001696:Biomechanical Phenomena; D008962:Models, Theoretical; D009010:Monte Carlo Method; D010578:Petroleum; D012623:Seawater; D014872:Water Movements
D010578:Petroleum