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My PhD Thesis, PDF 3MB - Stanford University

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? (1 )<br />

(1 )<br />

( 1) (1 )<br />

( r , k , ) cJ ( r ) s H ( r ) (A-3.2)<br />

o <br />

o <br />

(1)<br />

The first term cJ ( r ) represents the incoming wave. Constant c is determined by the<br />

o <br />

boundary conditions. Everywhere within the borehole 2<br />

( 1) 2<br />

J J 0 , even at r=0,<br />

o o<br />

since J o ( 0 ) =1, The second term s H o<br />

(1)<br />

(1 )<br />

( r ) is outgoing wave generated by the point<br />

<br />

source. It remains to determine the constant s . Substituting (A-3.2) and integrating<br />

both sides over a small area 2<br />

, we have<br />

Since<br />

s ( 2<br />

2 <br />

0<br />

0<br />

( 1)<br />

H ( x ) i o<br />

2<br />

ln<br />

<br />

x<br />

2<br />

integrating equation (A-3.3) gives<br />

where Green's Theorem<br />

4 s i F ( ) 1<br />

( 1) (1 ) 2 (1 )<br />

H H 0<br />

0<br />

with u 1 is used. From (A-3.4) we obtain<br />

<br />

- 154 -<br />

) rd dr F ( ) 1<br />

<br />

for x 0 ,<br />

. (A-3.3)<br />

for 0 , (A-3.4)<br />

( u 2<br />

G G 2<br />

G u<br />

u ) dS ( u<br />

S<br />

G ) dL (A-3.5)<br />

L n n

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