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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