Experiments have been performed on a laminar flat plate boundary layer
undergoing transition to turbulence. Reproducible disturbances were i
ntroduced via a loudspeaker embedded at some upstream location and the
ir evolution over the plate measured using hot-wire anemometry. A new
technique has been used to estimate the number of nonlinearly independ
ent modes in the reconstructed phase portraits. Nonlinear maps were th
en fitted that explicitly model the spatial evolution of disturbances.
These maps are consistent with classical linear stability theory for
small disturbances, and give rise to 'Smale horse-shoe' like behaviour
for larger amplitude disturbances. Thus a mechanism for generating ch
aos has been uncovered.