Biomedical Engineering Reference
In-Depth Information
1
3
(
σ
=
σ
+
σ
+
σ
δ
In Eq. (6.1),
zz
) denotes the mean normal stress
2)
and
ij
the
m
xx
yy
δ
=
=
Kronecker tensor (
ij
is equal to 1 if
i
j
,and0if
i
j
). Furthermore, Einstein's
summation convention was used [7].
Equation (6.1) can be written with components in the following way as
σ
σ
σ
σ
m
00
0
s
xx
s
xy
s
xz
xx
xy
xz
σ
σ
σ
=
σ
0
+
s
xy
s
yy
s
yz
(6.2)
xy
yy
yz
m
σ
σ
σ
00
σ
s
xz
s
yz
s
zz
xz
yz
zz
m
ij
Stress tensor
σ
ij
Deviatoric tensor
s
ij
Hydrostatic tensor
σ
It can be seen that the elements outside the main diagonal, that is, the shear
stresses, are the same for the stress and the deviatoric stress tensors:
s
ij
=
σ
for
i
=
j
(6.3)
ij
s
ij
=
σ
−
σ
m
for
i
=
j
(6.4)
ij
The hydrostatic part of
σ
ij
has in the case of metallic materials (full dense materials),
for temperatures approximately under 0
.
3
·
T
kf
(
T
kf
: melting temperature), nearly
no influence on the occurrence of inelastic strains since dislocations slip only
under the influence of shear stresses. On the other hand, the hydrostatic stress has
a considerable influence on the failure or yielding behavior in the case of cellular
materials, in soil or damage mechanics.
6.2.2
Invariants
To ensure the independence of a stress-based description of physical phenomena
from the chosen coordinate system (objectiveness), it is meaningful to use a set
of independent tensor invariants instead of the stress tensor components
ij
.
These invariants are independent of the orientation of the coordinate system and
represent the physical content of the stress tensor. The so-called characteristic
equation
3)
det
σ
σ
ij
=
−
λδ
0
(6.5)
ij
or in components
σ
−
λσ
σ
xx
xy
xz
σ
σ
−
λσ
=
0
(6.6)
xy
yy
yz
σ
σ
σ
−
λ
xz
yz
zz
leads to the cubic equation
3
2
λ
−
I
1
(
σ
ij
)
λ
+
I
2
(
σ
ij
)
λ
−
I
3
(
σ
ij
)
=
0
(6.7)
2)
Also called the hydrostatic stress. In the
context of soil mechanics, also the pressure
p
=−
σ
m
is used. Be aware that some finite
element codes use this definition.
3)
det(
) denotes the determinant of a matrix
or tensor.
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