Civil Engineering Reference
In-Depth Information
The variance of
M
is then defined by
z
B
2
⎡
⎤
⎧
⎫
{
}
2
⎢
⎪
⎪
⎥
⎡
⎤
2
()
( )
()
( )
xEMxt
,
E
∫
Gxqxt x
,
σ
=
=
⋅
⎨
⎬
⎢
⎥
⎢
⎥
Mr
z
r
M
y
z
B
z
B
⎣
⎦
⎪
⎪
⎢
⎥
L
⎩
⎭
(7.17)
exp
⎣
⎦
()
()
( ) ( )
∫∫
GxGxEqxt
,
qxt
,
x x
=
⋅
⋅
⎡
⋅
⎤
⎣
⎦
M
1
M
2
y
1
y
2
1
2
z
z
L
exp
rendering a spatial and time domain averaging of the fluctuating cross sectional load.
Introducing Eq. 7.15 then this space and time domain averaging is given by
(
)
(
)
Eq x t q x t
⎡
,
,
⎤
⋅
=
⎣
⎦
y
1
y
2
2
VB
⎡
D
D
D
D
⎤
ρ
⎧
⎫⎧
⎫
⎛
⎞
⎛
⎞
⎛
⎞
ECu
2
CCw
′
2
Cu
CCw
′
+
−
⋅
+
−
⎨
⎬⎨
⎬
⎢
⎥
⎜
⎟
⎜
⎟
⎜
⎟
D
1
D
L
1
D
2
D
L
2
2
B
B
B
B
⎝
⎠
⎝
⎠
⎝
⎠
⎣
⎩
⎭ ⎩
⎭
⎦
(7.18)
(
)
(
)
(
)
(
)
where
. It is a usual
assumption in wind engineering that cross-covariance between different velocity
components is negligible, i.e. that
uuxt
1
,
,
uuxt
2
,
and
wwxt
1
,
,
wwxt
2
,
=
=
=
=
1
2
1
2
(
)
(
)
(
)
(
)
Euxt wxt
⎡
,
⋅
,
⎤ ⎡
=
Euxt wxt
,
⋅
,
⎤
⎦
≈
0
(7.19)
⎣
⎦ ⎣
1
2
2
1
in which case
(
)
(
)
Eq x t q x t
⎡
,
,
⎤
⋅
=
⎣
⎦
y
1
y
2
2
2
2
⎧
⎫
VB
D
D
⎛
ρ
⎞ ⎛
⎪
⎞
⎛
⎞
⎪
(
)
(
)
(
)
(
)
2
CEuxt
,
uxt
,
CCEwxt
′
,
wxt
,
⎡
⋅
⎤
+
−
⎡
⋅
⎤
⎨
⎬
⎜
⎟ ⎜
⎟
⎜
⎟
⎣
⎦
⎣
⎦
D
1
2
D
L
1
2
2
B
B
⎝
⎠ ⎝
⎠
⎝
⎠
⎪
⎪
⎩
⎭
(7.20)
Introducing (see chapters 2.2 and 3.3)
(
)
(
)
2
(
)
E ux t ux t
,
,
x
⎡
⋅
⎤
=
σρ Δ
⋅
⎣
⎦
1
2
u u
(7.21)
(
)
(
)
2
(
)
E wx t wx t
⎡
,
⋅
,
⎤
=
σ
⋅
ρ
Δ
x
⎣
⎦
1
2
w
w
where
ρ
and
ρ
are the covariance coefficients of the
u-
and
w-
components, and
uu
ww
where
x
=−
is spanwise separation, then
xx
Δ
12