Journal of Fluid Mechanics

The Korteweg-de Vries equation and water waves. Part 2. Comparison with experiments

Joseph L.  Hammack a1 and Harvey  Segur a2
a1 W. M. Keck Laboratory of Hydraulics and Water Resources, California Institute of Technology, Pasadena
a2 Department of Mathematics, Clarkson College of Technology, Potsdam, New York

Article author query
hammack jl   [Google Scholar] 
segur h   [Google Scholar] 


The Korteweg-de Vries (KdV) equation is tested experimentally as a model for moderate amplitude waves propagating in one direction in relatively shallow water of uniform depth. For a wide range of initial data, comparisons are made between the asymptotic wave forms observed and those predicted by the theory in terms of the number of solitons that evolve, the amplitude of the leading soliton, the asymptotic shape of the wave and other qualitative features. The KdV equation is found to predict accurately the number of evolving solitons and their shapes for initial data whose asymptotic characteristics develop in the test section of the wave tank. The accuracy of the leading-soliton amplitudes computed by the KdV equation could not be conclusively tested owing to the viscous decay of the measured wave amplitudes; however, a procedure is presented for estimating the decay in amplitude of the leading wave. Computations suggest that the KdV equation predicts the amplitude of the leading soliton to within the expected error due to viscosity (12%) when the non-decayed amplitudes are less than about a quarter of the water depth. Indeed, agreement to within about 20% is observed over the entire range of experiments examined, including those with initial data for which the non-decayed amplitudes of the leading soliton exceed half the fluid depth.

(Published Online March 29 2006)
(Received September 10 1973)