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The work for the whole body of volume V then amounts to
( x , y , ... , γ yz )
W i
=−
x d
+ σ
y d
+···+ τ
yz d
γ
)
dV
x
y
yz
V
(
0 , 0 ,
...
0
)
ij
σ T d dV
=−
σ
=−
ij d
ij dV
(2.6)
V
0
V
0
with [Chapter 1, Eqs. (1.3) and (1.6)]
σ =
τ yz ] T
σ 23 ] T
[
σ x
σ y
σ z
τ xy
τ xz
=
[
σ 11
σ 22
σ 33
σ 12
σ 13
(2.7)
11 22 33 γ 12 γ 13 γ 23 ] T
The generalized Hooke's law takes the form [Chapter 1, Eqs. (1.34) and (1.35)]
yz ] T
=
[
xx
yy
zz
2
xy
2
xz
2
=
[
σ ij =
E ijkl kl
or σ =
E , so that for elastic bodies
1
2
1
2
T E dV
W i
=−
E ijkl
kl dV
=−
ij
V
V
1
2
1
2
σ T dV
=−
V σ
ij dV
=−
(2.8)
ij
V
where σ T
E T .
For a three-dimensional linear elastic body for which the strain energy is equal to but
opposite in sign to the work of the internal forces,
T
= T E T
= (
E )
and, because E is symmetric, E
=
1
2
1
2
T E dV
U i
=−
W i
=
U 0
()
dV
=
E ijkl
kl dV
=
(2.9)
ij
V
V
V
2 T E is the specific potential of a unit volume or the strain energy density .
With a symmetric matrix E , U 0 has the quadratic form
1
in which U 0
() =
1
2 T E
U 0
() =
G
23
2 γ
ν
1
2
11
2
22
2
33
2
2
12
2
13
2
=
+
+
+
ν ( 11 + 22 + 33 )
+
+ γ
+ γ
(2.10)
1
2
Here, it has been assumed that the material is isotropic, and E is taken from Eq. (1.34). A
quadratic function which is never negative for arbitrary values of the variables is called a
positive definite (quadratic) function. Such a function is zero only when each variable is zero.
As is shown in introductory mechanics of solids textbooks for isotropic materials, the shear
modulus of elasticity G must be positive, and Poisson's ratio
ν
can vary between zero and
one half, i.e., G
5. Thus, the strain energy density of Eq. (2.10) is a positive
definite function in the strain components.
It is useful to visualize again the strain energy in terms of a stress-strain curve of an
element, such as an extension bar. From Eq. (2.4)
U 0
A =
>
0 , 0
ν
0
.
x
0 σ
x d
(2.11)
x
is the area under the curves of Fig. 2.2. The area above the curve would be x d
σ x . Using
integration by parts, it follows that
U 0
A
σ
= σ
σ
= σ
x d
x d
(2.12)
x
x
x
x
x
x
The area above the curve is referred to as the complement of the area U 0
/
A
.
Set
σ x
U 0
A
x d
σ
=
(2.13)
x
0
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