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Thus
a
2
−
b
2
ω
=
yz
(10)
a
2
+
b
2
The
δφ
terms of (2) appear as
∂
∂
∂ω
∂
z
2
∂ω
∂
y
2
G
φ
dV
x
δφ
y
+
+
z
−
−
m
x
δφ
dx
=
0
(11)
L
Rewrite this as
∂ω
∂
2
∂ω
∂
2
∂
∂
z
∂ω
∂
y
∂ω
∂
x
δφ
+
+
y
−
y
z
z
L
A
z
∂ω
∂
z
2
dA G
y
∂ω
∂
y
2
φ
+
y
−
y
+
+
dx
−
m
x
δφ
dx
=
0
(12)
L
The integral
∂ω
∂
2
∂ω
∂
2
dA
z
∂ω
∂
y
∂ω
∂
+
+
y
−
(13)
y
z
z
A
can be shown to be zero. To do so, use the displacement relationship
0
of Eq. (1.151), Green's integral theorem of Appendix II, and the surface condition of
Eq. (1.153). Introduce
J
of Eq. (1.154)
∂
2
ω/∂
y
2
+
∂
2
ω/∂
z
2
=
y
y
z
z
dA
−
∂ω
∂
+
∂ω
∂
J
=
+
(14)
z
y
A
into (12), giving
d
dx
δφ
GJ
d
dx
dx
−
m
x
δφ
dx
=
0
(15)
L
L
Integrate by parts and use appropriate boundary conditions to find
d
dx
dx
GJ
d
dx
L
δφ
=−
m
x
δφ
dx
(16)
L
or
dx
GJ
d
d
dx
=−
m
x
(17)
This is the traditional equation of motion for torsion of a rod.
If
ω
of (10) is inserted in (14)
a
3
b
3
π
J
=
(18)
a
2
+
b
2
The stresses become
2
zM
t
ab
3
φ
(
τ
xy
=
G
γ
xy
=−
G
z
+
∂ω/∂
y
)
=−
π
(19)
2
yM
t
a
3
b
φ
(
−
τ
=
γ
=−
+
∂ω/∂
)
=−
G
G
y
z
xz
xz
π
These example problems illustrate several interesting characteristics of the Ritz method,
especially that of its simplicity and preciseness. Also, when the trial functions span the
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