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TABLE 2.2
Global Forms of the Fundamental Equations and the Classical Variational Principles
A
B
The force (static) boundary
The kinematical equations and
conditions and the conditions of
displacement (kinematical)
equilibrium (Eq. 2.44)
boundary conditions (Eq. 2.70)
S p δ u T
V δ σ T
( p p )
dS
( Du )
dV
u T
D T σ +
p T
=
V δ
(
p V )
dV
=
S u δ
(
u
u
)
dS
Gauss' Integral (Divergence) Theorem
Gauss' Integral (Divergence) Theorem
C
D
The principle of virtual work
The principle of complementary
(Eq. 2.54)
virtual work (Eq. 2.78)
V δ u T p V dV
V δ σ T dV
T σ dV
S u δ p T u dS
V δ( Du )
+
V δ(
S p δ
u T p dS
u T p dS
D T σ )
p T u dS
S p δ
S u δ
u dV
+
=
0
=
0
C and D are usually written without the underlined terms and then require admissible
displacements and stresses, respectively.
Observe that a complete description in variational form of the solid is provided by sum-
ming, for example, Eqs. (A) and (B)
u T
D T σ
σ T
V δ
(
+
p V )
dV
+
V δ
(
Du
)
dV
(
A
+
B
=
AB
)
u T
p T
+
S p δ
(
p
p
)
dS
S u δ
(
u
u
)
dS
=
0
(2.86)
That is, this expression is equivalent to
D T σ +
p V =
0
in
V
(2.87a)
=
Du
in
V
(2.87b)
with boundary conditions for forces:
A T σ =
p
=
p
on
S p
(2.87c)
for displacements:
=
u
u
on
S u
(2.87d)
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