Geology Reference
In-Depth Information
On interchanging the indices k and l ,aswellas i and j ,wefind
u l u i
u j
t lk =−
t kl ,
u k t ij
=−
(1.135)
using relation (1.133). The antisymmetry of t ij is preserved in the transformation to
the new co-ordinates, giving t kl =−
t lk . Then,τ 1
t 23 2
t 31 3
t 12 . Replacing
=
=
=
1 , τ
2 , τ
3 and the antisymmetric compon-
the antisymmetric components of t ij by τ
ents of t ij by τ 1 , τ 2 , τ 3 ,wefindthat
u 2
u 3
u 3
u 3
u 2 u 3
u 3 u 3
u 2 u 2
u 2 u 1
u 3 u 1
u 2 u 3
τ 1
1
2
=
τ
+
τ
u 1
u 3
u 2 u 2
u 3 u 2
u 2 u 1
3
+
τ
,
u 2
u 1
u 3
u 1
u 3 u 3
u 1 u 3
u 3 u 2
u 3 u 1
u 1 u 1
u 3 u 3
τ 2
1
2
=
τ
+
τ
(1.136)
u 1
u 1
u 3 u 2
u 1 u 2
u 3 u 1
3
+
τ
,
u 2
u 2
u 3
u 2
u 1 u 3
u 2 u 3
u 1 u 2
u 1 u 1
u 2 u 1
u 1 u 3
τ 3
1
2
=
τ
+
τ
u 1
u 2
u 1 u 2
u 2 u 2
u 1 u 1
3
+
τ
.
cients of the transformation law (1.36) for the covariant components
of a vector may be abbreviated as
The coe
a ij = u j
u i .
(1.137)
These may be regarded as the elements of a 3
×
3matrix,
u 1
/∂ u 1
u 2
/∂ u 1
u 3
/∂ u 1
u 1
/∂ u 2
u 2
/∂ u 2
u 3
/∂ u 2
A
=
.
(1.138)
u 1
/∂ u 3
u 2
/∂ u 3
u 3
/∂ u 3
Let C be the matrix of cofactors of the determinant,
, of the matrix A (1.138),
with elements c ij . Then, the transformation (1.136) of the quantitiesτ
|
A
|
j to the quant-
ities τ i may be written
τ i
j
=
c ij τ
.
(1.139)
The inverse of the matrix A is given by
C
A 1
B T
=
| =
,
(1.140)
|
A
 
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