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My PhD Thesis, PDF 3MB - Stanford University

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x ( r , z ) are used. Since there exist only P and SV waves in this radially symmetric<br />

problem, the displacement u can be written as (see Appendix A-1)<br />

u ( r , z, t ) (e ) , (2.2)<br />

where and are P wave and S wave potentials, respectively. Substituting equation<br />

(2.2) into the elastodynamic equation (2.1) we obtain (see Appendix A-2)<br />

??<br />

( r ) ( z )<br />

,<br />

r<br />

(2.3a)<br />

<br />

0 . (2.3b)<br />

( 2 ) 2<br />

( 2<br />

r 2 ) ??<br />

Equations (2.3a) and (2.3b) apply to each separate layer. These equations plus the<br />

application of boundaries at each interface constitute our mathematical problem. It is<br />

easier to solve this problem in k domain, because partial differential equations (2.3a)<br />

and (2.3b) in k domain become ordinary differential equations in r. Through the<br />

Fourier transform pair<br />

f<br />

? i t ik z<br />

(r , k , ) f (r , z , t )e dtdz<br />

f ( r , z , t ) <br />

<br />

1<br />

<br />

<br />

4 2<br />

<br />

<br />

<br />

<br />

<br />

<br />

<br />

<br />

<br />

?<br />

( i t ik z )<br />

f ( r, k , ) e d dk<br />

we can transform a function from z t domain to k domain and vice versa. From<br />

equation (2.3) we obtain the elastodynamic equations in k domain as<br />

d 2 ? ( j )<br />

dr 2<br />

1<br />

r<br />

d ? ( j )<br />

<br />

dr<br />

( j )<br />

( k <br />

2<br />

k 2<br />

) ? ( j)<br />

<br />

- 28 -<br />

,<br />

F ( )<br />

,<br />

( r )<br />

( j )<br />

( j)<br />

( 2 ) r<br />

, (2.4a)

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