TY - GEN
T1 - Coupling of NWT and large-eddy simulation for wave-induced sediment transport
AU - Harris, Jeffrey C.
AU - Grilli, Stephan T.
PY - 2010/9/10
Y1 - 2010/9/10
N2 - We present the validation and application of a numerical model for the simulation of wave-induced sediment transport. Our approach is a oneway coupling of an inviscid flow model (i.e., a Numerical Wave Tank based on potential flow theory; NWT) to a Navier-Stokes solver, to simulate near bottom wave-induced turbulent boundary layer flows. Only two-dimensional incident wave fields have been considered so far (i.e., long-crested swells), while the near-field wave-induced turbulent flow and sediment transport are fully three-dimensional. Good results are obtained for steady streaming velocities when applying open boundary conditions (i.e., zero velocity gradient), a quarter-wavelength from the edge of the domain without the assumption of periodicity. For turbulent test cases, we solve the Navier-Stokes equations using a large-eddy simulation using an approximate (log-layer) wall boundary condition and a dynamic Smagorinsky subgrid scale model. After validating the model hydrodynamic predictions, we simulate wave-induced sediment transport over an idealized rippled bed, and find reasonable agreement with laboratory results for oscillatory flows over full-scale sand ripples. Both idealized and more realistic test cases are presented.
AB - We present the validation and application of a numerical model for the simulation of wave-induced sediment transport. Our approach is a oneway coupling of an inviscid flow model (i.e., a Numerical Wave Tank based on potential flow theory; NWT) to a Navier-Stokes solver, to simulate near bottom wave-induced turbulent boundary layer flows. Only two-dimensional incident wave fields have been considered so far (i.e., long-crested swells), while the near-field wave-induced turbulent flow and sediment transport are fully three-dimensional. Good results are obtained for steady streaming velocities when applying open boundary conditions (i.e., zero velocity gradient), a quarter-wavelength from the edge of the domain without the assumption of periodicity. For turbulent test cases, we solve the Navier-Stokes equations using a large-eddy simulation using an approximate (log-layer) wall boundary condition and a dynamic Smagorinsky subgrid scale model. After validating the model hydrodynamic predictions, we simulate wave-induced sediment transport over an idealized rippled bed, and find reasonable agreement with laboratory results for oscillatory flows over full-scale sand ripples. Both idealized and more realistic test cases are presented.
KW - Computational fluid dynamics
KW - Hybrid model coupling
KW - Large eddy simulation
KW - Sand ripples
KW - Sediment transport
KW - Steady streaming
KW - Wave-induced oscillatory flows
UR - https://www.scopus.com/pages/publications/77956322356
M3 - Conference contribution
AN - SCOPUS:77956322356
SN - 9781880653777
T3 - Proceedings of the International Offshore and Polar Engineering Conference
SP - 578
EP - 585
BT - Proceedings of the 20th (2010) International Offshore and Polar Engineering Conference, ISOPE-2010
T2 - 20th International Offshore and Polar Engineering Conference, ISOPE-2010
Y2 - 20 June 2010 through 25 June 2010
ER -