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6
Linear Elast icity
6.1
Elasticity, Hooke’s Law, Strain Energy
Elastic behavior is characterized by the following two conditions: (1) where
the stress in a material is a unique function of the strain, and (2) where the
material has the property for complete recovery to a “natural” shape upon
removal of the applied forces. If the behavior of a material is not elastic, we
say that it is
inelastic
. Also, we acknowledge that elastic behavior may be
linear
. Figure 6-1 shows geometrically these behavior patterns
by simple stress-strain curves, with the relevant loading and unloading paths
indicated. For many engineering applications, especially those involving
structural materials such as metals and concrete, the conditions for elastic
behavior are realized, and for these cases the theory of elasticity offers a very
useful and reliable model for design.
Symbolically, we write the constitutive equation for elastic behavior in its
most general form as
or
non-linear
()
=
G
ε
(6.1-1)
is any one of the various
strain tensors we introduced earlier. However, for the response function
where
G
is a symmetric tensor-valued function and
ε
G
in this text we consider only that case of Eq 6.1-1 for which the stress is a
linear
function of strain. Also, we assume that, in the deformed material, the
displacement gradients are everywhere small compared with unity. Thus, the
distinction between the Lagrangian and Eulerian descriptions is negligible, and
following the argument of Eq 4.7-3 we make use of the infinitesimal strain
tensor defined in Eq 4.7-5, which we repeat here:
=
=
u
X
u
x
u
X
u
x
1
2
1
2
1
2
(
)
j
j
ε
=
i
+
i
+
uu
+
(6.1-2)
ij
i,j
j,i
j
i
j
i
809236664.011.png 809236664.012.png 809236664.013.png 809236664.014.png
 
FIGURE 6.1
Uniaxial loading-unloading stress-strain curves for (a) linear elastic; (b) nonlinear elastic; and
(c) inelastic behavior.
Within the context of the above assumptions, we write the constitutive
equation for linear elastic behavior as
σ
=
C
ε
or
=
C
ε
(6.1-3)
ij
ijkm
km
where the tensor of elastic coefficients
= 81 components. However,
due to the symmetry of both the stress and strain tensors, it is clear that
C
has 3
4
ijkm
C
=
C
=
C
(6.1-4)
ijkm
jikm
ijmk
which reduces the 81 possibilities to 36 distinct coefficients at most.
809236664.001.png
by a consideration of the
elastic constitutive equation when expressed in a rotated (primed) coordinate
system in which it has the form
We may demonstrate the tensor character of
C
′ = ′
σ
C
ε
(6.1-5)
ij
ijpn pn
But by the transformation laws for second-order tensors, along with Eq 6.1-3,
′ =
σ
aa
σ
=aaC
ε
ij
iq js qs
iq js qskm km
=
aaC a a
ε
iq js qskm pk nm pn
which by a direct comparison with Eq 6.1-5 provides the result
C ijpn
′ =
aaa a C
(6.1-6)
iq js pk nm qskm
that is, the transformation rule for a fourth-order Cartesian tensor.
In general, the
C
coefficients may depend upon temperature, but here
ijkm
we assume
(constant temper-
ature) conditions. We also shall ignore strain-rate effects and consider the
components
adiabatic
(no heat gain or loss) and
isothermal
to be at most a function of position. If the elastic coefficients
are constants, the material is said to be
C
ijkm
These constants are
those describing the elastic properties of the material. The constitutive law
given by Eq 6.1-3 is known as the
homogeneous.
generalized Hooke’s law.
For certain purposes it is convenient to write Hooke’s law using a single
subscript on the stress and strain components and double subscripts on the
elastic constants. To this end, we define
σ
=
σ
σ
=
σ
=
σ
11
1
23
32
4
σ
=
σ
σ
=
σ
=
σ
(6.1-7
a
)
22
2
31
13
5
σ
=
σ
σ
=
σ
=
σ
33
3
12
21
6
and
ε
=
ε
2
ε
= 2
ε
=
ε
11
1
23
32
4
ε
=
ε
2
ε
= 2
ε
=
ε
(6.1-7
b
)
22
2
31
13
5
ε
=
ε
2
ε
= 2
ε
=
ε
33
3
12
21
6
809236664.002.png
where the factor of two on the shear strain components is introduced in
keeping with Eq 4.7-14. From these definitions, Hooke’s law is now written
σ
=
C
ε
or
=
C
ε
(6.1-8)
α
αβ
β
with Greek subscripts having a range of six. In matrix form Eq 6.1-8 appears
as
σ
σ
σ
σ
σ
σ
CCCCCC
CCCCCC
CCCCCC
CCCCCC
CCCCCC
CCCCCC
ε
ε
ε
ε
ε
ε
1
11
12
13
14
15
16
1
2
21
22
23
24
25
26
2
3
31
32
33
34
35
36
3
=
(6.1-9)
4
41
42
43
44
45
46
4
5
51
52
53
54
55
56
5
6
61
62
63
64
65
66
6
does not constitute a tensor.
In view of our assumption to neglect thermal effects at this point, the
energy balance Eq 5.7-13 is reduced to the form
We point out that the array of the 36 constants
C
αβ
u= 1
ρ σ
D
ij ij
(6.1-10
a
)
which for small-deformation theory, by Eq 4.10-18, becomes
u= 1
˙
˙
ρ σε
(6.1-10
b
)
ij ij
The internal energy
u
in these equations is purely mechanical and is called
the
(per unit mass). Recall now that, by the continuity equation
in Lagrangian form,
strain energy
ρ
=
ρ
J
and also that to the first order of approximation
o
≈+
u
X
u
X
J
= det
F
=
det
δ
+
i
1
i
(6.1-11)
iA
A
A
Therefore, from our assumption of small displacement gradients, namely
u
/
X
<< 1, we may take
J
1 in the continuity equation to give
ρ
=
ρ
, a
i
A
0
constant in Eqs 6.1-10.
For elastic behavior under the assumptions we have imposed, the strain
energy is a function of the strain components only, and we write
u
=
u
(
ε
)
(6.1-12)
ij
809236664.003.png 809236664.004.png
 
so that
∂ε
u
˙
˙
u=
ε
(6.1-13)
ij
ij
and by a direct comparison with Eq 6.1-10
b
we obtain
1
ρ σ
∂ε
u
=
(6.1-14)
ij
ij
The
strain energy density,
W
(strain energy per unit volume) is defined by
W
=
ρ
u
(6.1-15)
0
and since
, a constant, under the assumptions we have made, it follows
from Eq 6.1-14 that
ρ
=
ρ
0
σρ
u
∂ε
W
=
=
(6.1-16)
ij
∂ε
ij
ij
It is worthwhile noting at this point that elastic behavior is sometimes
defined on the basis of the existence of a strain energy function from which
the stresses may be determined by the differentiation in Eq 6.1-16. A material
defined in this way is called a
material. The stress is still a unique
function of strain so that this energy approach is compatible with our earlier
definition of elastic behavior. Thus, in keeping with our basic restriction to
infinitesimal deformations, we shall develop the linearized form of Eq 6.1-16.
Expanding
hyperelastic
W
about the origin, we have
() +
()
2
WW W
0
∂ε ∂ε
W
0
() =
1
2
() +
ε
0
ε
εε
+
L
(6.1-17)
ij
ij
ij
km
∂ε
ij
ij
km
and, from Eq 6.1-16,
== () +
() +
2
W
0
∂ε ∂ε
W
0
∂ε
W
σ
ε
L
(6.1-18)
ij
km
∂ε
ij
ij
ij
km
It is customary to assume that there are no residual stresses in the unstrained
state of the material so that
= 0. Thus, by retaining only the
linear term of the above expansion, we may express the linear elastic con-
stitutive equation as
σ
= 0 when
ε
ij
ij
() =
2
∂ε ∂ε
W
0
σ
=
ε
C
ε
(6.1-19)
ij
km
ijkm km
ij
km
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