Deconvolution of down-going seismic wavefields
A method for reducing effects of free surface multiple reflections from seismic signal measurements. The measurements result from seismic energy imparted into the Earth's subsurface from collocated measurements related to pressure and vertical component of motion in response to the imparted seismic energy. The method includes entering as input to a computer the measurements related to pressure and vertical component of motion. In the computer, a down-going component of the measurements is determined. An impulse response of the Earth in the absence of a free surface from the down-going component is determined.
1. A method for reducing effects of free surface multiple reflections in seismic signal measurements, the measurements resulting from seismic energy imparted into the Earth's subsurface from collocated measurements of pressure and vertical component of motion in response to the imparted seismic energy, the method comprising:
entering as input to a computer the measurements related to pressure and vertical component of motion;
in the computer, determining a down-going component of the measurements without using an up-going component of the measurements;
in the computer, determining an impulse response of the Earth to the imparted seismic energy in the absence of a free surface from the down-going component; and
at least one of storing and displaying the determined impulse response.
2. The method of claim 1 wherein the measurements related to pressure comprise measurements of a time derivative of the pressure.
3. The method of claim 2 wherein the measurements of a time derivative of pressure comprise hydrophone measurements.
4. The method of claim 1 wherein the measurements related to vertical component of motion comprise particle velocity measurements.
5. The method of claim 4 wherein the particle velocity measurements comprise geophone measurements.
6. The method of claim 1 further comprising, in the computer, transforming the collocated measurements related to pressure and vertical component of motion in response to the imparted seismic energy into the frequency-wavenumber domain, and transforming the determined impulse response to the time-space domain.
7. The method of claim 1 further comprising filtering the determined impulse response of the Earth by a filter representing a band-limited monopole seismic energy source.
8. The method of claim 1 wherein the seismic energy is imparted by a source proximate the surface of a body of water.
9. The method of claim 1 wherein the measurements related to pressure and vertical component of motion in response to the imparted seismic energy are made by sensors disposed proximate the bottom of a body of water.
10. The method of claim 1 wherein the down-going component of the measurements is determined by linear decomposition.
11. A method for seismic surveying, comprising:
actuating a seismic energy source to impart seismic energy into subsurface formations;
making collocated measurements related to pressure and vertical component of motion in response to the imparted seismic energy;
entering as input to a computer the measurements related to pressure or time derivative of pressure, and vertical component of motion;
in the computer, determining a down-going component of the measurements without using an up-going component of the measurements;
in the computer, determining an impulse response of the Earth to the imparted seismic energy in the absence of a free surface from the down-going component; and
at least one of storing and displaying the determined impulse response.
12. The method of claim 11 wherein the measurements related to pressure comprise measurements of a time derivative of the pressure.
13. The method of claim 12 wherein the measurements of the time derivative comprise hydrophone measurements.
14. The method of claim 11 wherein the measurements related to vertical component of motion comprise particle velocity measurements.
15. The method of claim 14 wherein the particle velocity measurements comprise geophone measurements.
16. The method of claim 11 further comprising, in the computer, transforming the collocated measurements related to pressure and vertical component of motion in response to the imparted seismic energy to the frequency-wavenumber domain, and transforming the determined impulse response to the time-space domain.
17. The method of claim 11 further comprising filtering the determined impulse response of the Earth by a filter representing a band-limited monopole seismic energy source.
18. The method of claim 11 wherein the seismic energy is imparted by a source proximate the surface of a body of water.
19. The method of claim 11 wherein the measurements related to pressure and vertical component of motion in response to the imparted seismic energy are made by sensors disposed proximate the bottom of a body of water.
20. The method of claim 11 wherein the down-going component of the measurements is determined by linear decomposition.
21. A computer program stored in a non-transitory computer readable medium, the program having logic operable to cause a programmable computer to perform acts comprising:
accepting as input to the computer collocated measurements related to pressure and vertical component of motion resulting from seismic energy imparted into the Earth's subsurface;
determining a down-going component of the measurements without using an up-going component of the measurements;
determining an impulse response of the Earth to the imparted seismic energy in the absence of a free surface from the down-going component; and
at least one of storing and displaying the determined impulse response.
22. The computer program of claim 21 wherein the measurements related to pressure comprise measurements of a time derivative of the pressure.
23. The computer program of claim 22 wherein the measurements of a time derivative comprise hydrophone measurements.
24. The computer program of claim 21 wherein the measurements related to vertical component of motion comprise particle velocity measurements.
25. The computer program of claim 24 wherein the particle velocity measurements comprise geophone measurements.
26. The computer program of claim 21 further comprising logic operable to cause the computer to perform transforming the collocated measurements related to pressure and vertical component of motion in response to the imparted seismic energy to the frequency-wavenumber domain, and transforming the determined impulse response to the time-space domain.
27. The computer program of claim 21 further comprising logic operable to cause the computer to perform filtering the determined impulse response of the Earth by a filter representing a band-limited monopole seismic energy source.
28. The computer program of claim 21 wherein the seismic energy is imparted by a source proximate the surface of a body of water.
29. The computer program of claim 21 wherein the measurements related to pressure and vertical component of motion in response to the imparted seismic energy are made by sensors disposed proximate the bottom of a body of water.
30. The computer program of claim 21 wherein the down-going component of the measurements is determined by linear decomposition.