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PROCESS TX2FK
Parameters, alphabetically:
coords etime lprint nprestk nxpad
stime twinlen weight xwinlen
Document Date: 5 July 2007
version 2.1 a.j. harding
Modifications:
November 2006 - Change TWINLEN from time to number of samples.
- Change TWINLEN preset to 25 samples.
July 2007 - Only sort traces by range when nprestk > 2
- Abort if < 2 traces in tx.
- Allow up to 32K samples per time trace.
PROCESS TX2FK transforms data from the TX (time-space) domain into the
F-K (frequency-wavenumber) domain by performing a 2-D FFT. The input
is a set of normal (t-x) seismic traces and the output is a transformed
set of F-K traces. The transformed output traces are in rectangular
form unless polar form (amplitude and phase) is requested.
The frequencies within each output trace are ordered from -Nyq to 0 to
Nyq. Each output trace contains a power of 2 number of samples. The
traces are ordered in wavenumber from 0 to K (Nyquist). Data in polar
form are ordered with the modulus followed by the argument.
The sample interval is in hundreds of microhertz in order to prevent
truncation problems. e.g. an SEG-Y trace header interval value of 610
is really 610/10,000. or .0610. See doc/fk.forum for further discussion.
The input traces must be sorted by increasing range (SEG-Y header
word 10) and must be separated uniformly. DELTA X must be positive
and must be constant. The only exception is when "super-gathers"
are to be used (see parameter nprestk).
Any SIOSEIS process may follow TX2FK, but care should be taken that it
makes sense! The imaginary part of data in rectangular coordinates may
be omitted from plot by decimating by a factor of 2.
The steps used in the F-K transformation are:
1.) Each trace is windowed temporally in order to minimize edge effects
along the time trace.
2.) The data are transposed so that all the data of constant times are
adjacent. This sorts the data by x rather than t (or f).
3.) The 'range' traces are zero padded. Effectively adding dummy traces
to the end of the dataset. The data must be padded to a power of 2,
but additional padding may be desirable for migration etc. A user
minimum number of dead traces is specified by nxpad. The data are
also windowed in x if desired.
4.) The complex FFT is performed, transforming x to k, or from space to
wavenumber.
5.) The data are transposed back to ordering by time.
6.) The forward FFT is performed, converting time to frequency. The
maximum number of samples in time is 8192 real samples.
7.) The data are converted to polar coordinates if requested. Data in
the fk domain may be processed by any other seismic process in
SIOSEIS.
The run time of TX2FK is governed by the number of traces, including pads,
and the trace length, including pads. Both dimensions are a power of 2,
so transforming 1500 points takes as long as 2000 points (2048 being the
closest larger power of 2).
The frequency-wavenumber domain is discussed in a paper "A Review of the
Two-Dimensional Transform and Its Use in Seismic Processing" by
D.W. March and A.D.Bailey in the "First Break", January 1983.
Each parameter list must be terminated with the word END. The entire set
of TX2FK parameters must be terminated by the word END.
THE PARAMETER DICTIONARY
--- --------- ----------
STIME - The start time of the data for the entire data set. Any trace
that has an initial time (delay) greater than STIME will be zero
padded so that the data starts at STIME . Any trace that has a
delay less than stime will be shortened.
Preset = the delay of the first trace.
ETIME - The end time of the data for the entire data set. Data in excess
of ETIME will be omitted from the transformation.
Preset = the last time of the first trace.
NXPAD - The number of dummy traces to insert at both ends of the seismic
line. PROCESS FKMIGR needs dummy traces in order to prevent
"wrap around".
Preset = 10
TWINDOW - The type of window to apply before computing the temporal fft.
= HAMM, Hamming
= HANN, Hanning
= GAUS, Gaussian
= BART, Bartlett (triangular)
= RECT, rectangular (box car - no window)
= BLAC, Blackman
= EBLA, exact Blackman
= BLHA, Blackman-Harris
Preset=HANN e.g. window rect
TWINLEN - The window length, in samples. A window length of zero causes
the entire time domain trace to be windowed. A non zero length
indicates that winlen data will be modified at both ends of
each trace.
Preset = 25 e.g. winlen 50
XWINDOW - Same as twindow but it windows the data by range.
Preset = RECT ( No windowing of ranges )
XWINLEN - The window length in number of traces. A window length of zero
causes the entire set of ranges to be windowed. A non-zero
length causes that number of traces to be tapered at the
binning and end.
Preset = 10
COORDS - The coordinates of the output trace.
= RECT, Rectangular coordinates. The output trace will be complex.
The trace values will consist of real and imaginary pairs. The
frequency dimension runs from 0 to Nyquist (pi) then the
negative frequencies back to 0, as output from the FFT. The
number of samples in the output frequency trace is a power of
two. The k dimension is also ordered as it comes directly out
of the FFT, 0 to Nyquist followed by the most negative k.
= POLAR, Polar coordinates. The first half of the output trace
will be the amplitude spectrum and the second half of the trace
will be the phase spectrum, each ordered 0 to Nyquist back to 0.
The k dimension is reordered so that the first trace is the
negative Nyquist, then increasing to 0, then increasing to the
positive Nyquist. The total number of traces output is a power
of two plus 1.
= POLARU, "user friendly" polar coordinates. This produces output
data as a series of wavenumber traces running from -Nyq -> +Nyq
and only positive frequencies in polar form (magnitude followed
by phase). This format is useful if it is desired to look at
the FK data using for example a contouring program. The data are
not used internally in this form but is converted on input/output
from SIOSEIS.
Preset = RECT e.g. coords POLAR
OHDRPATH - If processes TX2FK and FK2TX are called in the same job then
the original TX headers will be used as the trace headers of the
the processed TX data. This will preserve all RP/Shot numbering
as well as GMT information. However, if these two processes are
done in separate jobs then the user may specify a permanent disk
file to hold the original TX headers. This filename can then be
given to FK2TX when the inverse transform is done.
PATH1 & PATH2 - Before TX2FK transforms the input traces it accumulates
them them in a scratch datafile. The size of this file is the
number of input traces prior to padding in range * the sample
length of each trace (etime - stime) prior to padding in time.
The size of the data after transformation is equal to the number
of traces * trace length after padding of each to the nearest
power of 2. This is stored in a second scratch dataset after
which the first scratch file is deleted. If there is a FK2TX in
the procs list then it will use this second scratch file as its
first scratch file. The default location of these files is
implementation dependent and may be of insufficient size. The
PATH parameters allow the user to specify the location of the
two scratch files.
PATH1 - The location of the first scratch file.
PATH2 - The location of the 2nd scratch file. Since this is the same as
the first scratch file used by FK2TX (if present) it should be
given only here or in FK2TX. If contradictory definitions are
given the first on processed will be used.
NPRESTK - The number of rps to use in each fk transformation. Each rp is
terminated with a -1 in SEG-Y trace header word 51. Processes
SORT and GATHER set this "end-of-sort" flag. Shot data may set
this flag with process INPUT or DISKIN parameter NTRGAT. The data
are sorted by increasing range prior to transforming x to k.
Process fk2tx will automatically "unsort" the data into the
original order when nprestk is greather than 1.
END - Terminates each parameter list.
Copyright (C) the Regents of the University of California
All Rights Reserved
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Go to SIOSEIS introduction.