Introduction to Vectors and Tensors Vol 2 (Bowen 246). - Index of
Introduction to Vectors and Tensors Vol 2 (Bowen 246). - Index of Introduction to Vectors and Tensors Vol 2 (Bowen 246). - Index of
334 Chap. 9 • EUCLIDEAN MANIFOLDS a ( ) ˆ c a T x T ( x ) = δ (46.9) c b b for all x ∈U1∩U 2. It follows from (46.4) and (46.7) that A = T ⋅⋅⋅ T Aˆ (46.10) ˆb b 1 ˆ q a1... aq a1 aq b1... bq where A ˆ = A ( eˆ ,..., eˆ ) (46.11) b1... bq b1 bq Equation (46.10) is the transformation rule for the anholonomic components of A . Of course, (46.10) is a field equation which holds at every point of U1∩U2∩ U . Similar transformation rules for the other components of A can easily be derived by the same type of argument used above. We define the physical components of A , denoted by A a1 ,..., aq , to be the anholonomic components of A relative to the field of orthonomal basis { g i } whose basis vectors g are unit i vectors in the direction of the natural basis vectors g i of an orthogonal coordinate system. Let ( , x ) U by such a coordinate system with g = 0, i ≠ j. Then we define 1 ˆ ij g ( x) g ( x) g ( x ) (no sum) (46.12) i = i i at every x ∈U 1 . By (44.39), an equivalent version of (46.12) is g x = g x g x (46.13) 12 ( ) i( ) ( ii( )) (no sum) i Since { } i g is orthogonal, it follows from (46.13) and (44.39) that { i } g is orthonormal: g ⋅ g = δ a b ab (46.14)
Sec. 46 • Anholonomic and Physical Components 335 as it should, and it follows from (44.41) that ⎡1 g11( x) 0 ⋅ ⋅ ⋅ 0 ⎤ ⎢ 0 1 g22( x) 0 ⎥ ⎢ ⎥ ⎢ ⋅ ⋅ ⋅ ⎥ ij ⎡ ⎣g ( x) ⎤= ⎦ ⎢ ⎥ ⎢ ⋅ ⋅ ⋅ ⎥ ⎢ ⋅ ⋅ ⋅ ⎥ ⎢ ⎥ ⎣ 0 0 ⋅ ⋅ ⋅ 1 gNN ( x) ⎦ (46.15) This result shows that g can also be written i g ( x) g x x g x ( g ( x)) i 12 i ( ) = = ( g ( )) ( ) (no sum) i ii 12 ii (46.16) Equation (46.13) can be viewed as a special case of (46.7), where ⎡1 g11 0 ⋅ ⋅ ⋅ 0 ⎤ ⎢ ⎥ ⎢ 0 1 g22 0 ⎥ ⎢ ˆ b ⋅ ⋅ ⋅ ⎥ ⎡Ta ⎤= ⎢ ⎥ ⎣ ⎦ ⎢ ⋅ ⋅ ⋅ ⎥ ⎢ ⎥ ⎢ ⋅ ⋅ ⋅ ⎥ ⎢ 0 0 1 g ⎥ ⎣ ⋅ ⋅ ⋅ NN ⎦ By the transformation rule (46.10), the physical components of A are related to the covariant components of A by (46.17) ( ) −12 ≡ ( g , g ,..., g ) = 1 2... 1 2 aa ⋅⋅⋅ 1 1 a 1... (no sum) aa a a a q aq qaq a aq A A g g A (46.18) Equation (46.18) is a field equation which holds for all x ∈U . Since the coordinate system is orthogonal, we can replace (46.18) 1 with several equivalent formulas as follows:
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334 Chap. 9 • EUCLIDEAN MANIFOLDS<br />
a<br />
( ) ˆ c a<br />
T x T ( x ) = δ<br />
(46.9)<br />
c b b<br />
for all x ∈U1∩U 2. It follows from (46.4) <strong>and</strong> (46.7) that<br />
A = T ⋅⋅⋅ T Aˆ<br />
(46.10)<br />
ˆb<br />
b<br />
1 ˆ q<br />
a1... aq a1 aq b1...<br />
bq<br />
where<br />
A ˆ = A ( eˆ ,..., eˆ<br />
)<br />
(46.11)<br />
b1...<br />
bq<br />
b1<br />
bq<br />
Equation (46.10) is the transformation rule for the anholonomic components <strong>of</strong> A . Of course,<br />
(46.10) is a field equation which holds at every point <strong>of</strong> U1∩U2∩<br />
U . Similar transformation rules<br />
for the other components <strong>of</strong> A can easily be derived by the same type <strong>of</strong> argument used above.<br />
We define the physical components <strong>of</strong> A , denoted by<br />
A<br />
a1 ,..., aq<br />
, <strong>to</strong> be the anholonomic<br />
components <strong>of</strong> A relative <strong>to</strong> the field <strong>of</strong> orthonomal basis { g i } whose basis vec<strong>to</strong>rs g are unit<br />
i<br />
vec<strong>to</strong>rs in the direction <strong>of</strong> the natural basis vec<strong>to</strong>rs g<br />
i<br />
<strong>of</strong> an orthogonal coordinate system. Let<br />
( , x )<br />
U by such a coordinate system with g = 0, i ≠ j. Then we define<br />
1 ˆ<br />
ij<br />
g ( x) g ( x) g ( x ) (no sum)<br />
(46.12)<br />
i<br />
=<br />
i<br />
i<br />
at every x ∈U 1<br />
. By (44.39), an equivalent version <strong>of</strong> (46.12) is<br />
g x = g x g x (46.13)<br />
12<br />
( )<br />
i( ) (<br />
ii( )) (no sum)<br />
i<br />
Since { } i<br />
g is orthogonal, it follows from (46.13) <strong>and</strong> (44.39) that { i }<br />
g is orthonormal:<br />
g ⋅ g = δ<br />
a b ab<br />
(46.14)