Wind Energy Handbook. Michael Barton Graham

Wind Energy Handbook - Michael Barton Graham


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is important to note that where the incident velocity varies spatially, as here, W takes the value that would exist at the effective position of the bound vortex representing the local blade circulation excluding its own induced velocity.

      Consequently,

      so

      If, therefore, a is to take everywhere the optimum value (1/3), the circulation must be uniform along the blade span, and this is a condition for optimised operation.

      To determine the blade geometry, that is, how should the chord size vary along the blade and what pitch angle β distribution is necessary, neglecting the effect of drag, we must return to Eq. (3.52) with CD set to zero:

StartFraction upper W squared Over upper U Subscript infinity Baseline Superscript 2 Baseline EndFraction upper B StartFraction c Over upper R EndFraction upper C Subscript l Baseline sine phi equals 8 pi lamda mu squared a prime left-parenthesis 1 minus a right-parenthesis

      substituting for sinϕ gives

StartFraction upper B Over 2 pi EndFraction StartFraction c Over upper R EndFraction equals StartStartFraction 4 lamda mu squared a prime OverOver StartFraction upper W Over upper U Subscript infinity Baseline EndFraction upper C Subscript l Baseline EndEndFraction

      Hence

      The parameter λμ is the local speed ratio λr and is equal to the tip speed ratio where μ = 1.

      In off‐optimum operation, the axial inflow factor is not uniformly equal to 1/3; in fact, it is not uniform at all.

Graph depicts the variation of blade geometry parameter with local speed ratio. Graph depicts the variation of inflow angle with local speed ratio.

      which, for optimum operation, is

      Close to the blade root the inflow angle is large, which could cause the blade to stall in that region. If the lift coefficient is


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