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The pressure component (P) and the vertical component (Z)
of the receiver gather are both in the frequency domain.
The available data are the hydrophone component (P) and the non-calibrated geophone component
(,C is the calibration factor we need to compute):
| |
|
| (2) |
The initial source wavefield is given as follows:
The propagated upgoing and downgoing wavefields at the water-bottom surface
are, respectively,
| |
|
| (4) |
where , is the water depth and
v is the water velocity. From equations (3)
and (4) the propagated source at the water-bottom surface is as follows:
| |
(5) |
The calibration methodology assumes that the source energy should
be zero after a time equal to the sum of the source-receiver propagation time
and the source duration, which is a few hundred milliseconds. Combining equations (2)
and (5) yields the following relation between the propagated source (S) and
the hydrophone (P) and geophone (Z) components:
where:
The propagated source vanishes after a certain period of time if the hydrophone and
geophone are calibrated. This corresponds to finding C such that the propagated source
(S) has minimum energy after a period of time:
| |
(7) |
The solution for this simple least-squares problem is as follows:
| |
(8) |
where is a small constant to avoid dividing by zero.
The filter C [equation (8)] is for a single trace. To obtain a filter for
the entire gather, we compute the filter C for each trace and average them.
Figure 6 shows the hydrophone component of the receiver gather (left), the geophone
component of the receiver gather (center) and the calibrated geophone (left).
cal
Figure 6 From left to right: hydrophone, geophone and
calibrated geophone.
Next: Deghosting
Up: Frequency domain methodology
Previous: Frequency domain methodology
Stanford Exploration Project
5/23/2004