Select to expand quote
Andrew / Geelong said.
Do small Deltas ETC that are proven fast at Lake George ETC create any lift at all!!
ANDY H GEELONG
I think I can answer one part of your question: Short weed fins by nature tend to be very stiff. Tip flex is not sufficient to be a meaningful source of spanwise or, in this case, 'vertical' lift. Spanwise flows down a raked leading edge do produce vertical lift. However, it takes a chunk of energy to change the direction of the water flow from straight across the fin, to angle it down the leading edge. This energy requirement is manifested as drag.
A delta like fin at very high angles of attack can develop a leading edge vortex running down the fin. When sailing, it feels like the fin is almost spun out, but hasn't quite let go. In this state, the fin does produce some 'vertical' lift, but it is intensely draggy. Leading edge vortex flow is unsteady, so unless you are sailing in smooth water the vortex is likely to join with the trailing edge low pressure area and ventilate the entire surface, that is, spin out.
A large radius leading raked edge does have a speedboat hull like effect and does want to ride up over the water, again, vertical lift. The effect of this is double-edged. Increasing the fin drag, but decreasing the board drag can be very effective (e.g. foiling) but only up to a point. Increased frontal area on a fin increases the drag exponentially, so at higher speed the relative board drag becomes low, and the fin feels like it has hit a speed wall.
Just on a small tangent, flow across a windsurfing fin needs to be mostly attached to provide lateral lift. It is usually turbulent, but it can, under a special set of circumstances, be laminar. At windsurfing speeds, the inertia effects of the water's mass dictate the flow around the fin. Viscous effects such as creating laminar flow are overwhelmed. A perfectly smooth fin, in perfectly smooth water conditions, will achieve laminar flow for about 2 cm from the leading edge, even less as the speed increases or there is a ripple on the water. Or a butterfly takes off in the Amazon forest. The transition from laminar flow to turbulent flow is more unstable and violent the longer the flow resists tripping to turbulent flow. The severity of the transition to turbulent flow when windsurfing can induce small cavitation bubbles that migrate downstream and provide a pathway for leading and trailing edge low pressure areas and/or surface ventilation to join. Sudden sheet cavitation is the result. (e.g. spin out). In reality, a perfectly smooth fin is almost impossible to achieve, whereas chord length, chord width, and leading edge radius are potent influences on flow and pressure. Similarly, given fins are surface piercing, the effect of wingspan and ventilation is also important. But that is all another story, and methinks I have hijacked this thread too much already.