This paper shows the results of an experimental work on the spilling type breaking flow field produced by a hydrofoil positioned in a uniform current. From the examination of the Laser Doppler Anemometer results downstream of the hydrofoil a flow field similar to a mixing layer, close to the breaking zone, and a flow field similar to a wake were found. The conclusions that can be drawn by the studies conducted can be summarized as follows: (i) downstream of the hydrofoil it is possible to distinguish two regions of flow, namely one immediately downstream of the hydrofoil, including spilling characterized by a mixing of water and air, and one downstream of the same spilling; (ii) in first of the aforementioned regions the flow is similar to that of a mixing layer, while, in the downstream region, it shows conditions similar to a wake; (iii) the experiments furnish information on the turbulence characteristics in the two regions, and extract the zone where the wake effect can be considered negligible; (iv) the time-averaged free surface height presents a decreasing trend from the wake origin
Experimental study of the flow field with spilling type breaking / Mossa, Michele. - In: JOURNAL OF HYDRAULIC RESEARCH. - ISSN 0022-1686. - 46:Suppl. 1(2008), pp. 81-86. [10.1080/00221686.2008.9521942]
Experimental study of the flow field with spilling type breaking
MOSSA, Michele
2008
Abstract
This paper shows the results of an experimental work on the spilling type breaking flow field produced by a hydrofoil positioned in a uniform current. From the examination of the Laser Doppler Anemometer results downstream of the hydrofoil a flow field similar to a mixing layer, close to the breaking zone, and a flow field similar to a wake were found. The conclusions that can be drawn by the studies conducted can be summarized as follows: (i) downstream of the hydrofoil it is possible to distinguish two regions of flow, namely one immediately downstream of the hydrofoil, including spilling characterized by a mixing of water and air, and one downstream of the same spilling; (ii) in first of the aforementioned regions the flow is similar to that of a mixing layer, while, in the downstream region, it shows conditions similar to a wake; (iii) the experiments furnish information on the turbulence characteristics in the two regions, and extract the zone where the wake effect can be considered negligible; (iv) the time-averaged free surface height presents a decreasing trend from the wake originI documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.

