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Annual Report 2000 - WIT

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ò<br />

Ý<br />

ã þ ¥¿åLK<br />

D<br />

û<br />

Ý<br />

ò<br />

ýÝ<br />

þ =OF å Þ ü ã<br />

, ü<br />

ã<br />

û ¥ å Þ K<br />

, <br />

§<br />

ä¨= Þ §<br />

ô<br />

ý<br />

þ<br />

Ý<br />

Ý<br />

ý<br />

Þ<br />

=OF þ<br />

can be expressed by , ã þ ==<br />

and ã ,<br />

þ<br />

þ == Þ ã<br />

û<br />

ñ<br />

ý<br />

ã þ =E<br />

Ý<br />

ñ¦=<br />

ñ ò<br />

<br />

<br />

þ<br />

<br />

û<br />

207<br />

as they are shown in Figure 1. We ò é<br />

insert ò and into the parabolic expansion (1)<br />

respectively. Building the sum and the difference of the resulting expressions yields<br />

the following result:<br />

Þâò é<br />

ò ñ<br />

(6)<br />

ú²ñ¦= å<br />

9 ã ==„å ò é ô ò<br />

For the hyperbolic form we find a similar solution. ò é<br />

Inserting ò ,<br />

to<br />

ú€ñ¦=wå<br />

ò Ý<br />

Þâò Ý é<br />

ã == å ò Ý<br />

Ý 9<br />

ò Ý é Þ<br />

= <br />

ò Ý<br />

ú Ý<br />

and ò ñ<br />

into (4) leads<br />

(7)<br />

ó î=<br />

ó î Ý<br />

= Þ<br />

ò ñ ó î=<br />

B The - and ã ú€ñ<br />

-components ã of and can be found in the same way by varying 4<br />

respectively . Varying both îE<br />

and leads to ã =E<br />

; ã EF<br />

and ã F=<br />

follow accordingly.<br />

The determination of the îF - and î= -components of îE ø•ñ<br />

is straightforward: instead<br />

ã<br />

B 5<br />

and ã<br />

ò ñ ó î Ý<br />

of varying the receiver position we use different source positions. For the -, BHB -, 5 B -<br />

and 5G5 5<br />

-components of ã<br />

B<br />

both source and receiver positions have to be varied. But this<br />

does not yet give us the -components. Unless we compute also traveltimes for sources<br />

at different depths – which we do not intend to – another approach is needed. At this<br />

4<br />

point we make use of the eikonal equation to express the -component of the slowness<br />

vector 4 ø•ñ<br />

as ã<br />

ø•ñFqåJI Þ ø Ý ñ¦= Þ ø Ý (8)<br />

ñ¦E Ý <br />

where is the velocity at the source, provided that the source lies in the top surface<br />

,<br />

of the model. Otherwise we have to insert a sign in (8). Since second order traveltime<br />

derivatives are also first order derivatives of slownesses we can ã rewrite ã and to<br />

ø¥ §<br />

äHM § ¤N<br />

ú/ §<br />

䨥OM § %<br />

ø9¥ §<br />

î¨#M § ¤<br />

(9)<br />

åLK<br />

<br />

If we now substitute ø•ñF in equation (9) by (8) we can compute the second order derivatives<br />

of ò with respect to äF and îF from the already known 5 -B -matrix elements and<br />

derivatives of the velocity. Since we assume the velocity field to be smooth, the velocity<br />

derivatives can be determined with a second order FD operator on the coarse grid.<br />

To give an example the matrix ã<br />

þ =E<br />

element as<br />

¦<br />

<br />

<br />

ø•ñ¦=<br />

ø•ñF<br />

ø•ñ¦E<br />

ø•ñF<br />

(10)<br />

ø•ñF<br />

This expression will not yield a result for ã þ =OF<br />

if ø•ñF equals zero. This case has, however,<br />

no practical relevance for the applications that the method was developped for. The<br />

ã and is straightforward.<br />

derivation of the remaining 4 -components of ã<br />

, ë

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