Environmental Engineering Reference
In-Depth Information
d 2
dt r P / B
d W
dt
x r P / B + 2W x d
a P (a) = a B (a) +
dt r P / B (b ) + W x (W x r P / B ) +
(11-18)
The indicated operations of Equation (11-18) must be carried out, and the results must then
be transformed to the b coordinate system and linearized. This tedious activity gives the
expressions for the acceleration components in the x p -y p -z p coordinates. For the small-
deformation theory of this analysis, there is no difference between the x p -y p -z p and h-z-x
coordinate systems with respect to structural equations. For convenience, therefore, we will
use the same h-z-x notation for the accelerations as for the relative velocities. This gives
a P , h
a P , z
a P ,x
é
ê ë
a P =
(11-19a)
a P , h = - s q p ( r W 2 b 0 + 2 f W rc y + f rs y + v W 2 c q p )
- zW 2 c q p s q p - hW 2 c q p
(11-19b)
a P , z = - c q p ( r W 2 b 0 + 2 fW rc y + f rs y) - v W 2 c q p
- z W 2 s q p - hW 2 s q p c q p + v
(11-19c)
a P , x = - r W 2 2W vs q p
(11-19d)
where
a P,h , a P,z , a P,x = components of the acceleration vector at an arbitrary point P within the
blade, in the normal, chordwise, and spanwise directions, respectively
(m/s 2 )
Aerodynamic Loading
Referring to Figure 6-1, the lift and drag forces on an airfoil section are given by
dL = 1
2 r C L c V rel d x
(11-20a)
1
2 r C D cV rel d x
(11-20b)
dD =
where
dL = increment of lift force, normal to the relative wind (N)
dD = increment of drag force, parallel to the relative wind (N)
r = air density (kg/m 3 )
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