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In measuring acoustic field vector properties either complete or partial cancellation between ambient noise energy flux and the oppositely directed one,radiated,for instance,by tone or noise-shaped point source can be found.In that case there is no matter coherent or incoherent fields interact.The phenomenon of interest is named compensation of opposing energy fluxes.The paper is focused on interaction between vertical component of the surface noise energy flux and that of bottom-reflected noise-shaped interfering signal from on-water source in the deep open ocean.Bottom-reflected weak broadband interfering signal measures the extent of resultant compensation.As the vertical projection of the signal energy flux makes the interference maximum,its power appears to be comparable to that of the surface noise and complete compensation takes place at a given frequency.Once it is the interference minimum, just partial compensation can be found.No compensation was observed for co-directional energy fluxes.
In measuring acoustic field vector properties either complete or partial cancellation between ambient noise energy flux and the oppositely directed one, radiated, for instance, by tone or noise-shaped point source can be found. That case there is no matter coherent or incoherent fields interact.The phenomenon of interest is named compensation of opposing energy fluxes. The paper is focused on interaction between vertical component of the surface noise energy flux and that of bottom-reflected noise-shaped interfering signal from on-water source in the deep open ocean .Bottom -reflicated broadband interferenceing signal measures the extent of resultant compensation. As the vertical projection of the signal energy flux makes the interference maximum, its power appears to be comparable to that of the surface noise and complete compensation takes place at a given frequency .Once it is the interference minimum, just partial compensation can be found. No compensation was observed for co-directional e nergy fluxes.