Marine time-lapse seismic surveying
View Patent ↗A method for making a time-lapse seismic survey in a marine environment, the method designed to eliminate multiple surface reflections and changes in sea state and conditions. Seismic sources and receivers are positioned at predetermined conditions for a first set of data in which at least two sets of seismic signals are recorded at each receiver, proximate in time, such that there are insignificant changes in the subsurface formation. At a later point in time the seismic source(s) and receiver(s) are positioned at the same place when the first seismic data set was generated. A seismic source emits a sound wave and the seismic receiver receives what will be called a “monitor signal” and the two-way water travel time is again determined. A model is then developed for the first and second seismic data sets in that includes the subsurface signal, changes in the subsurface signal and the effect of multiple reflections. A set of filter functions are then developed to filter out the multiple reflections based on the two-way water travel times of the first seismic data set. The first seismic data set, the second seismic data set and the filter function are then used to calculate the differences in the subsurface layers over the elapsed period of time between the two seismic data sets.
1. A method of marine time-lapse seismic surveying the subsurface, using a seismic source and a seismic receiver system comprising at least one seismic receiver, the steps comprising:
(a) positioning the seismic source at a source location having a predetermined position, and positioning the at least one seismic receiver of the seismic receiver system at a receiver location having predetermined position;
(b) recording for these source and receiver locations for each seismic receiver a set of at least two repeat signals obtained from the seismic receiver in response to a set of at least two sound waves emitted by the seismic source, wherein the at least two sound waves are emitted at different sea states but so closely in time that differences in the repeat signals due to changes in the subsurface can be ignored, and measuring the two-way water travel times when recording the repeat signals;
(c) positioning after a predetermined period of time the seismic source and the at least one seismic receiver at the source and receiver locations of step (a), recording for each seismic receiver a monitor signal from the seismic receiver in response to a sound wave emitted by the seismic source, and measuring the two-way water travel time when recording the monitor signal;
(d) assuming a model for the signal that includes the subsurface signal, differences in the subsurface signals due to changes in the subsurface, and the contributions of surface multiple reflections;
(e) determining a set of filter functions that enable eliminating the surface multiple reflections, which filter function(s) are functions of the measured two-way water travel times at the position of the seismic source of step (a);
(f) calculating for each receiver the estimated differences in the subsurface signals from the repeat signals, the monitor signal and the filter function(s), which estimated difference is a measure of changes in the subsurface signal caused by changes in the target layer in the time elapsed between recording the repeat signals and recording the monitor signal; and
(g) outputting the estimated difference.
2. A method of marine time-lapse seismic surveying the subsurface, using a seismic source and a seismic receiver system comprising at least one seismic receiver located at a predetermined receiver location, the steps comprising:
(a) positioning the seismic source at a source location having a predetermined position;
(b) recording for this source location for each seismic receiver a set of at least two repeat signals obtained from the seismic receiver in response to a set of at least two sound waves emitted by the seismic source, wherein the at least two sound waves are emitted at different sea states but so closely in time that differences in the repeat signals due to changes in the subsurface can be ignored, and measuring the two-way water travel times when recording the repeat signals;
(c) positioning after a predetermined period of time the seismic source at the source location of step (a), recording for each seismic receiver a monitor signal from the seismic receiver in response to a sound wave emitted by the seismic source, and measuring the two-way water travel time when recording the monitor signal;
(d) assuming a model for the signal that includes the subsurface signal, differences in the subsurface signals due to changes in the subsurface, and the contributions of surface multiple reflections;
(e) determining a set of filter functions that enable eliminating the surface multiple reflections, which filter function(s) are functions of the measured two-way water travel times at the position of the seismic source of step (a);
(f) calculating for each receiver the estimated differences in the subsurface signals from the repeat signals, the monitor signal and the filter function(s), which estimated difference is a measure of changes in the subsurface signal caused by changes in the target layer in the time elapsed between recording the repeat signals and recording the monitor signal; and
(g) outputting the estimated difference.
3. A method of marine time-lapse seismic surveying the subsurface, using a seismic source located at a predetermined source location and a seismic receiver system comprising at least one seismic receiver located at a predetermined receiver location, the steps comprising:
(a) recording for each seismic receiver a set of at least two repeat signals obtained from the seismic receiver in response to a set of at least two sound waves emitted by the seismic source, wherein the at least two sound waves are emitted at different sea states but so closely in time that differences in the repeat signals due to changes in the subsurface can be ignored, and measuring the two-way water travel times when recording the repeat signals;
(b) recording after a predetermined period of time for each seismic receiver a monitor signal from the seismic receiver in response to a sound wave emitted by the seismic source, and measuring the two-way water travel time when recording the monitor signal;
(c) assuming a model for the signal that includes the subsurface signal, differences in the subsurface signals due to changes in the subsurface, and the contributions of surface multiple reflections;
(d) determining a set of filter functions that enable eliminating the surface multiple reflections, which filter function(s) are functions of the measured two-way water travel times;
(e) calculating for each receiver the estimated differences in the subsurface signals from the repeat signals, the monitor signal and the filter function(s), which estimated difference is a measure of changes in the subsurface signal caused by changes in the target layer in the time elapsed between recording the repeat signals and recording the monitor signal; and
(f) outputting the estimated difference.
4. The method according to claim 1 , further comprising repeating steps (c) through (g).
5. The method according to claim 2 , further comprising repeating steps (c) through (g).
6. The method according to claim 3 , further comprising repeating steps (b) through (f).
7. The method according to claim 1 , wherein the signals are passed through a band-pass filter such that the pass frequencies are limited by frequencies for which a pole occurs in the Fourier Transform of the filter function, before the estimated differences are calculated.
8. The method according to claim 2 , wherein the signals are passed through a band-pass filter such that the pass frequencies are limited by frequencies for which a pole occurs in the Fourier Transform of the filter function, before the estimated differences are calculated.
9. The method according to claim 3 , wherein the signals are passed through a band-pass filter such that the pass frequencies are limited by frequencies for which a pole occurs in the Fourier Transform of the filter function, before the estimated differences are calculated.