Geography Reference
In-Depth Information
Tab l e 1 . 3
Various deformation tensors of the first kind
Definitions Author Comments
E
1
=C
l
=S
l
R
∗
G
r
RS
l
=J
l
G
r
J
l
Cauchy
(
1889
,
1890
) (“left Cauchy-Green”) if G
r
=I,then
C
l
=S
l
=J
l
J
l
E
2
=C
r
=S
r
R
∗
G
l
RS
r
=J
r
G
l
J
r
Green
(
1839
) (“right Cauchy-Green”) if G
l
=I,then
C
r
=S
r
=J
r
J
r
E
3
=C
l
G
−
1
l
Grafarend
(
1995
) (“left-right Cauchy-Green”)
if G
l
=I,then
E
3
=C
l
E
4
=C
r
G
−
1
Grafarend
(
1995
) (“right-left Cauchy-Green”)
if G
r
=I,
then E
4
=C
r
r
E
5
=G
l
C
−
1
Grafarend
(
1995
) (“inverse left-right Cauchy-Green”)
Finger
(
1894a
)ifG
l
=I,
then E
5
=E
−
1
l
3
E
6
=G
r
C
−
1
Grafarend
(
1995
) (“inverse right-left Cauchy-Green”)
Piola
(
1836
), if G
r
=I,
then E
6
=E
−
1
r
4
E
7
=C
m/
2
l
Λ
m
1
,Λ
m
∼{
2
}
Seth
(
1964a
,
b
)(
m
∈
Z,m
=0)
m
=2:E
7
=E
1
E
8
=InC
l
∼{
In
Λ
1
,
In
Λ
2
}
−
Hencky
(
1928
)
E
9
=C
m/
r
∼{
λ
m
1
,λ
m
2
}
Seth
(
1964a
,
b
)
m
=2:E
9
=E
2
E
10
=InC
r
∼{
In
λ
1
,
In
λ
2
}
Hencky
(
1928
)
−
E
11
=E
l
=
2
(C
l
−
G
l
)
Cauchy
(
1889
,
1890
) (“left Euler-Lagrange”)
if G
l
=I,then
E
l
=
2
(C
l
−
I)
E
12
=E
r
=
2
(G
r
−
C
r
)
Almansi
(
1911
) (“right Euler-Lagrange”)
if G
r
=I,then
E
r
=
2
−
(I
C
r
)
E
13
=E
l
G
−
1
l
=
2
(C
l
G
−
1
l
−
I)
Grafarend
(
1995
) (“left-right Euler-Lagrange”)
if G
l
=I,then
E
13
=E
l
E
14
=E
r
G
−
1
=
2
C
r
G
−
1
(I
−
)
Grafarend
(
1995
) (“right-left Euler-Lagrange”)
if G
r
=I,
then E
14
=E
r
r
r
E
15
=
2
(C
−
1
l
G
−
l
)
−
Karni and Reiner
(
1960
)
if G
l
=Ithen
E
15
=
2
(C
−
1
l
−
I)
Definitions
Author
Comments
E
16
=
2
(G
−
r
−
C
−
1
r
)
Karni and Reiner
(
1960
)
if G
r
=Ithen
E
16
=
2
C
−
1
r
(I
−
)
E
17
=G
l
E
−
1
Grafarend
(
1995
) (“inverse left-right Euler-Lagrange”) if G
l
=I,then
E
17
=E
−
1
l
l
E
18
=G
r
E
−
1
Grafarend
(
1995
) (“inverse right-left Euler-Lagrange”) if G
r
=I,then
E
18
=E
−
1
r
r
E
19
=E
m/
2
l
K
m/
2
1
,K
m/
2
2
∼{
}
Seth
(
1964a
,
b
)(
m
∈
Z,m
=0)
m
=2:E
19
=E
11
E
20
=
2
In E
l
Hencky
(
1928
)
−
E
21
=E
m/
r
∼{
K
m/
2
1
,K
m/
2
2
}
Seth
(
1964a
,
b
)
m
=2:E
21
=E
12
E
22
=
2
In E
r
Hencky
(
1928
)
−
cos
Ψ
l
=
U
1
|
U
2
=
cos
Ψ
r
=
u
1
|
u
2
=
versus
(1.133)
U
1
U
2
g
μν
u
1
u
2
G
MN
√
G
AB
U
2
√
G
ΓΔ
U
1
√
g
αβ
u
1
u
2
√
g
γδ
u
1
u
2
=
=
.
U
1
U
2
The second additive measure of deformation is the
angular shear
or the
angle of shear
(Σ
l
is of
type “left” and Σ
r
is of type “right”, respectively)
Σ
l
=Σ:=
Ψ
l
−
Ψ
r
versus
Σ
r
=
σ
:=
Ψ
r
−
Ψ
l
.
(1.134)
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