We report on the observation
of gravity-capillary wave turbulence on the surface of a fluid
in a high-gravity environment. By using a large-diameter
centrifuge, the effective gravity acceleration is tuned up to 20
times the Earth gravity. The transition frequency between the
gravity and capillary regimes is thus increased up to one decade
as predicted theoretically. A frequency power-law wave spectrum
is observed in each regime and is found to be independent of the
gravity level and of the wave steepness. While the timescale
separation required by weak turbulence is well verified
experimentally regardless of the gravity level, the nonlinear
and dissipation timescales are found to be independent of the
scale, as a result of the finite size effects of the system
(large-scale container modes) that are not taken currently into
account theoretically.