Benjamin-Feir instability of nonlinear gravity-capillary waves is studied e
xperimentally. The experimental results are compared with computations perf
ormed for values of wavelength and steepness identical to those employed in
the experiments. The theoretical approach is based on the Zakharov nonline
ar equation which is modified here to incorporate weak viscous dissipation.
Experiments are performed in a wave flume which has an accurately controll
ed wavemaker for generation of the carrier wave, as well as an additional i
ndependent conical wavemaker for generation of controlled three-dimensional
disturbances. The approach adopted in the present experimental investigati
on allows therefore the determination of the actual boundaries of the insta
bility domain, and not just the most unstable disturbances. Instantaneous s
urface elevation measurements are performed with capacitance-type wave gaug
es. Multipoint measurements make it possible to determine the angular depen
dence of the amplitude of the forced and unforced disturbances, as well as
their variation along the tank. The limits of the instability domains obtai
ned experimentally for each set of carrier wave parameters agree favourably
with those computed numerically using the model equation. The numerical st
udy shows that application of the Zakharov equation, which is free of the n
arrow-band approximation adopted in the derivation of the nonlinear Schrodi
nger (NLS) equation, may lead to qualitatively different results regarding
the stability of nonlinear gravity-capillary waves. The present experiments
support the results of the numerical investigation.