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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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