Seismic sources are generally devices that generate acoustic energy. One use of seismic sources is in marine seismic surveying in which the seismic sources may be employed to generate acoustic energy that travels downwardly through water and into subsurface rock. After interacting with the subsurface rock, e.g., at boundaries between different subsurface layers, some of the acoustic energy may be returned toward the water surface and detected by specialized sensors (e.g., hydrophones, geophones, etc.). The detected energy may be used to infer certain properties of the subsurface rock, such as structure, mineral composition and fluid content, thereby providing information useful in the recovery of hydrocarbons.
Most of the seismic sources employed today in marine seismic surveying are of the impulsive type, in which efforts are made to generate as much energy as possible during as short a time span as possible. The most commonly used of these impulsive-type sources are air guns that typically utilize compressed air to generate acoustic energy. Other examples of impulsive-type sources include explosives and weight-drop impulse sources. The frequency content of these impulsive-type sound sources typically in use today is controllable only to a small degree. As a result, different sound sources may be selected for the generation of different frequency ranges based on the surveying needs. Notably, these impulsive-type sources also have limited acoustic energy output in the very low frequency band from 1-10 Hz. However, it is well known that as sound waves travel through water and through subsurface geological structures, higher frequency sound waves may be attenuated more rapidly than lower frequency sound waves, and consequently, lower frequency sound waves can be transmitted over longer distances through water and geological structures than higher frequency sound waves. Thus, efforts have been undertaken to develop sound sources that can operate at low frequencies.
These drawings illustrate certain aspects of some of the embodiments of the present invention and should not be used to limit or define the invention.
It is to be understood that the present disclosure is not limited to particular devices or methods, which may, of course, vary. It is also to be understood that the terminology used herein is for the purpose of describing particular embodiments only, and is not intended to be limiting. All numbers and ranges disclosed herein may vary by some amount. Whenever a numerical range with a lower limit and an upper limit is disclosed, any number and any included range falling within the range are specifically disclosed. Although individual embodiments are discussed, the invention covers all combinations of all those embodiments. As used herein, the singular forms “a”, “an”, and “the” include singular and plural referents unless the content clearly dictates otherwise. Furthermore, the word “may” is used throughout this application in a permissive sense (i.e., having the potential to, being able to), not in a mandatory sense (i.e., must). The term “include,” and derivations thereof, mean “including, but not limited to.” The term “coupled” means directly or indirectly connected. If there is any conflict in the usages of a word or term in this specification and one or more patent or other documents that may be incorporated herein by reference, the definitions that are consistent with this specification should be adopted for the purposes of understanding this invention.
Embodiments relate generally to seismic sources for marine geophysical surveys. More particularly, embodiments relate to a seismic source that utilizes an external driver to energize the air in the seismic source for generation of acoustic energy.
With additional reference to
In this particular embodiment, the seismic source 12 may include components, such as a pair of base plates 20a and 20b. While not illustrated, springs and mass elements may be attached to the base plates 20a and 20b as desired for a particular application. In some embodiments, the base plates 20a and 20b may be generally planar. In particular embodiments, the base plates 20a and 20b may each be in the form of a flexible disk. In embodiments, the base plates 20a and 20b may each be flat, circular disks having substantially uniform thickness. However, other configurations, including both axially-symmetric and not, of the base plates 20a and 20b may be suitable for particular applications. By way of example, the base plates 20a and 20b may be rectangular, square, elliptical, or other suitable shape for providing the desired acoustic energy. The base plates 20a and 20b may be made from any of a variety of materials including materials comprising steel, aluminum, a copper alloy, glass-fiber reinforced plastic (e.g., glass-fiber reinforced epoxy), carbon fiber reinforced or other suitable flexible spring material. Examples of suitable copper alloys may include brass, beryllium, copper, phosphor bronze, or other suitable copper alloy. In some embodiments, the base plates 20a and 20b may comprise aluminum. The plates 20a and 20b may be made from the same or a different material. In particular embodiments, the base plates 20a and 20b may have a thickness from about 1 millimeter to about 12 millimeters or even greater. In general, the base plates 20a and 20b should have a thickness that allows sufficient deformation but withstand expected differential static pressures.
The base plates 20a and 20b may be secured together or otherwise positioned to provide the internal cavity 18 of the seismic source 12 between the base plates 20a and 20b. The base plates 20a and 20b may also be secured to one another in a manner that allows the base plates 20a and 20b to bend and create the desired acoustic energy. In particular embodiments, the base plates 20a and 20b may be coupled to another at their outer edges. In one non-limiting embodiment, the base plates 20a and 20b may be secured together by hoop 22, as illustrated on
The internal cavity 18 may also include ports, such as 24a, 24b, 24c, and 24d illustrated in
The internal cavity 18 may be configured to hold a volume of a fluid, which may be a gas, such as air or another compressible fluid or gaseous substance. The volume of fluid within the internal cavity 18 may be dependent on the volume of the internal cavity 18, which in turn would depend on the dimensions of the internal cavity 18 (e.g., diameter, length, height, etc.). The volume of fluid contained within the internal cavity 18 may serve, among other purposes, as a compliant medium to reduce any impedance to the vibration amplitude of the base plates 20a and 20b. In some embodiments, the entire volume of the internal cavity 18 may not be filled with the fluid. For example, other fluids such as oils, alcohols, water/glycol mixtures, etc., may be used in the internal cavity 18. In some embodiments, the volume of fluid within the internal cavity 18 may be pressurized. In marine applications, for example, pressuring and maintaining the volume of fluid within the internal cavity 18 at an ambient hydrostatic pressure at an operating water depth may protect the seismic source 12 from collapsing from ambient hydrostatic pressure.
In the embodiment illustrated in
Referring now to
In the embodiment illustrated in
In addition, more than one external driver 14 may be used and arranged in series or in parallel. By way of example,
The external driver 14 may be any suitable driver for generation of a pressure wave that energizes the fluid in the internal cavity 18 of the seismic source 12. In some embodiments, the external driver 14 may be an electroacoustic transducer for generation of acoustic energy. In non-limiting embodiments, the electroacoustic transducer may generate force by vibrating a portion of its surface. In other embodiments, the external driver 14 may be linear motor, such as a linear motor, which may be a linear magnetic motor that may be energized electrically. A suitable linear motor may include stationary electric coils and a magnetic component (e.g., a magnetic cylinder) that passes through a magnetic field generated by the stationary electric coils, or vice versa. An example embodiment with a linear motor is described in more detail below with respect to
With additional reference to
In the embodiment illustrated in
In the embodiment illustrated in
Referring now to
In the embodiment illustrated on
In the non-limiting embodiment illustrated in
With continued reference to
As discussed earlier, the apparatus 10 may include an external driver 14. In some embodiments, the apparatus 10 may include fluid resonance, for example, a resonating flow of fluid back and forth between the external driver 14 and the fluid reservoir 16. The fluid may resonate, for example, in response to an input of energy (e.g., applying a current to the voice coil 34 on
Specifically, when the external driver 14 includes a loudspeaker, the external driver 14 may include a voice coil 34, as illustrated on
The fluid resonance may be adjusted by adjusting at least one dimension of the conduit system 27. Because a fluid resonance of the volume flowing between the external driver 14 and the fluid reservoir 16 may be approximate as proportional to the square root of the cross-sectional area of the second conduit 42 divided by the length of the second conduit 42, given a particular change in a cross-sectional area and/or a length of the second conduit 42, a corresponding change in the resonance of the volume of fluid within the second conduit 42 may be approximated or determined. In non-limiting embodiments, a resonance frequency of the fluid resonating between the fluid reservoir 16 and the external driver 14 may be adjustable or tunable based on adjusting or varying (e.g., a cross-sectional area, a length, etc.) of the second conduit 42. Second conduit 42 may include at least one dimension that is adjustable to change, adjust, or tune a resonance frequency. In one embodiment, the dimension that is adjustable may be the length of the second conduit 42. In other embodiments, the dimension that is adjustable or tunable may include a width, a diameter, a cross-sectional area or other dimension of the second conduit 42, or combinations of any of these dimensions. While illustrated, the portion of the second conduit 42 that is adjustable may be disposed in the fluid reservoir 16. Alternatively, when the fluid resonance may be between the seismic source 12 and the external driver 14 at least one dimension of the first conduit 28 may be adjusted.
Referring now to
Apparatus 10 may further comprise support structure 48 for stack assembly 46, fluid reservoir 16, and external driver 14. Support structure 48 may be in form of a frame as illustrated or any other suitable device for supporting the components of the apparatus 10. In the illustrated embodiment, stack assembly 46 may be disposed below upper portion 50 of the support structure 48, whereas the fluid reservoir 16 and the external driver 14 may be disposed above the upper portion 50. However, the stack assembly, 46, fluid reservoir 16, and the external driver 14 may be positioned at different positions with respect to the support structure 48.
In this non-limiting embodiment, first conduit 28 may couple the external driver 14 to the stack assembly 46. First conduit 28 may be in a general vertical configuration, as illustrated. In the illustrated embodiment, first conduit 28 may comprise manifold conduits 44a, 44b, 44c, and 44d which may be coupled to each of manifolds 52a, 52b, 52c, and 52d, as illustrated on
Referring now to
The embodiment illustrated in
Referring now to
As illustrated, the marine survey system 86 may further comprise an apparatus 10 towed by the survey vessel 88 (or a different vessel) in the body of water 90. A source cable 96 may couple the apparatus 10 to the survey vessel 88. The apparatus 10 may be towed in the body of water 90 at a depth ranging from 0 meters to about 120 meters, for example, or even deeper. At selected times, the seismic source 12 (not in site) may be triggered, for example, by the recording system 92, to generate acoustic energy.
In some embodiments, the marine survey system 86 may further comprise at least one streamer 98 towed by the survey vessel 88 (or a different vessel) to detect the acoustic energy that originated from the seismic source 12 after it has interacted, for example, with formations 100 below the water bottom 102. As illustrated, both the apparatus 10 and the streamer 98 may be towed above the water bottom 102. The streamer 98 may contain seismic sensors 94 thereon at spaced apart locations. In some embodiments, more than one streamer 98 may be towed by the survey vessel 88, which may be spaced apart laterally, vertically, or both laterally and vertically. While not shown, some seismic surveys locate seismic sensors 94 on ocean bottom cables or nodes in addition to, or instead of, streamer 98. The seismic sensors 94 may be any type of seismic sensors 94 known in the art, including hydrophones, geophones, particle velocity sensors, particle displacement sensors, particle acceleration sensors, or pressure gradient sensors, for example. By way of example, the seismic sensors 94 may generate response signals, such as electrical or optical signals, in response to detected acoustic energy. Signals generated by the seismic sensors 94 may be communicated to the recording system 92. The detected energy may be used to infer certain properties of the subsurface rock, such as structure, mineral composition and fluid content, thereby providing information useful in the recovery of hydrocarbons.
In non-limiting embodiments, a geophysical data product indicative of certain properties of the subsurface rock may be produced from the detected energy. The geophysical data product may include processed seismic geophysical data and may be stored on a non-transitory, tangible computer-readable medium. The geophysical data product may be produced offshore (i.e. by equipment on a vessel) or onshore (i.e. at a facility on land) either within the United States or in another country. If the geophysical data product is produced offshore or in another country, it may be imported onshore to a facility in the United States. Once onshore in the United States, geophysical analysis may be performed on the data product.
Advantageously, the seismic sources 12 disclosed herein may display a low resonance frequency in the seismic frequency range of interest. In particular embodiments, the seismic sources 12 may display a resonance frequency (when submerged in water at a depth of from about 0 meters to about 300 meters or alternatively from about 30 meters to about 300 meters) in the seismic frequency range of interest between about 1 Hz to about 200 Hz. In alternative embodiments, the seismic sources 12 may display at least one resonance frequency (when submerged in water at a depth of from about 0 meters to about 300 meters or alternatively from about 30 meters to about 300 meters) between about 0.1 Hz and about 100 Hz and, alternatively, between about 0.1 Hz and about 10 Hz. In some embodiment, the seismic sources 12 may display at least one resonance frequency of about 10 Hz or lower (when submerged in water at a depth of from about 0 meters to about 300 meters or alternatively from about 30 meters to about 300 meters).
One of the many potential advantages of the systems and methods of the present invention, only some of which are disclosed herein, is that an increased pressure differential may be tolerated by the seismic source 12 by use of the external driver 14. For example, the tolerable pressure differential may increase from a few meters to +/−1 meter, thus enabling use of the seismic source 12 in rougher weather conditions with reduced burden on the static pressure compensation system. In addition, in some examples, the seismic source 12 may be more reliable in operation due to elimination of the fragile piezoelectric bodies, the bond between the piezoelectric bodies and base plates 20a, 20b, and the voltage required to energize the piezoelectric bodies. Another one of the many potential advantages of the systems and methods of the present invention may be that a seismic source 12 energized by the external driver 14 may be much less costly than use of the piezoelectric bodies while also having a potentially shorter development time to the commercial production. Seismic sources 12 without the piezoelectric bodies may also have less costly routine maintenance due to their reduced costs. Moreover, no special amplifiers may be required wherein multiple external drivers 14 may be wired in series/parallel combinations to provide the desired impedance. Additionally, it is believed that the output may be increased per seismic source 12, reducing system cost and size, wherein base plates 20, 20b that may be all aluminum, for example, may be able to be driven harder. Should there be a catastrophic failure of the static pressure compensation system or an event that causes the depth to change too quickly, less damage may occur if piezoelectric bodies are not used with potential repair only requiring only replacement of the benders and the electroacoustic transmitting transducers.
The foregoing figures and discussion are not intended to include all features of the present techniques to accommodate a buyer or seller, or to describe the system, nor is such figures and discussion limiting but exemplary and in the spirit of the present techniques.
The present application claims priority to U.S. provisional application No. 62/086,601, filed Dec. 2, 2014, the disclosure of which is incorporated herein by reference.
Number | Name | Date | Kind |
---|---|---|---|
3384868 | Brown | May 1968 | A |
3978940 | Bouyoucos | Sep 1976 | A |
3990034 | Abbott | Nov 1976 | A |
4185714 | Pascouet et al. | Jan 1980 | A |
4211301 | Mifsud | Jul 1980 | A |
4231112 | Massa | Oct 1980 | A |
4483411 | Mifsud | Nov 1984 | A |
4492285 | Fair | Jan 1985 | A |
4525645 | Shirley et al. | Jun 1985 | A |
4556963 | Hugus et al. | Dec 1985 | A |
4557348 | Mifsud | Dec 1985 | A |
4578784 | Mifsud | Mar 1986 | A |
4689997 | Windisch | Sep 1987 | A |
4739859 | Delano | Apr 1988 | A |
4753316 | Bouyoucos et al. | Jun 1988 | A |
4785430 | Cole | Nov 1988 | A |
4850449 | Cheung | Jul 1989 | A |
4853905 | Myers | Aug 1989 | A |
5016228 | Arnold et al. | May 1991 | A |
5050129 | Schultz | Sep 1991 | A |
5062089 | Willard | Oct 1991 | A |
5126979 | Rowe, Jr. et al. | Jun 1992 | A |
5206839 | Murray | Apr 1993 | A |
5225731 | Owen | Jul 1993 | A |
5233570 | Donskoy | Aug 1993 | A |
5302782 | Owen | Apr 1994 | A |
5579287 | Boucher | Nov 1996 | A |
5646380 | Vaage | Jul 1997 | A |
5694374 | Ripoll | Dec 1997 | A |
5757726 | Tenghamn et al. | May 1998 | A |
5757728 | Tenghamn et al. | May 1998 | A |
5959939 | Tenghamn et al. | Sep 1999 | A |
5978316 | Ambs | Nov 1999 | A |
6009047 | Barger | Dec 1999 | A |
6041888 | Tenghamn | Mar 2000 | A |
6076629 | Tenghamn | Jun 2000 | A |
6076630 | Ambs | Jun 2000 | A |
6085862 | Tenghamn | Jul 2000 | A |
6230840 | Ambs | May 2001 | B1 |
6173803 | Barger | Nov 2001 | B1 |
6404106 | Dale et al. | Jun 2002 | B1 |
6464035 | Chelminski | Oct 2002 | B1 |
6556510 | Ambs | Apr 2003 | B2 |
6606958 | Bouyoucos | Aug 2003 | B1 |
6624539 | Hansen et al. | Sep 2003 | B1 |
6711097 | Engdahl | Mar 2004 | B1 |
6851511 | Tenghamn | Feb 2005 | B2 |
7468932 | Tenghamn | Dec 2008 | B2 |
7539079 | Hoogeveen et al. | May 2009 | B2 |
7551518 | Tenghamn | Jun 2009 | B1 |
7562740 | Ounadjela | Jul 2009 | B2 |
7881158 | Tenghamn | Feb 2011 | B2 |
7926614 | Tenghamn et al. | Apr 2011 | B2 |
7929380 | Wei et al. | Apr 2011 | B2 |
7957220 | Howlid et al. | Jun 2011 | B2 |
7974152 | Tenghamn | Jul 2011 | B2 |
8050139 | Berstad | Nov 2011 | B2 |
8050867 | Johnson et al. | Nov 2011 | B2 |
8061471 | Wei | Nov 2011 | B2 |
8079440 | Laycock | Dec 2011 | B2 |
8081540 | Ross | Dec 2011 | B2 |
8094514 | Tenghamn | Jan 2012 | B2 |
8098542 | Hillesund et al. | Jan 2012 | B2 |
8102731 | Cambois | Jan 2012 | B2 |
8154176 | Karakaya et al. | Apr 2012 | B2 |
8167082 | Eick et al. | May 2012 | B2 |
8174927 | Hopperstad et al. | May 2012 | B2 |
8205711 | Hopperstad et al. | Jun 2012 | B2 |
8261875 | Eick et al. | Sep 2012 | B2 |
8331198 | Morozov et al. | Dec 2012 | B2 |
8335127 | Tenghamn | Dec 2012 | B2 |
8342288 | Eick et al. | Jan 2013 | B2 |
8400872 | Gulgne et al. | Mar 2013 | B2 |
8427901 | Lunde et al. | Apr 2013 | B2 |
8441892 | Morozov et al. | May 2013 | B2 |
8446798 | Tenghamn | May 2013 | B2 |
8630149 | Thompson et al. | Jan 2014 | B2 |
8634276 | Morozov et al. | Jan 2014 | B2 |
8670292 | Engdahl | Mar 2014 | B2 |
8804462 | Barbour et al. | Aug 2014 | B2 |
8909480 | Wei | Dec 2014 | B2 |
8971152 | Chelminski | Mar 2015 | B2 |
9348042 | Sallas | May 2016 | B2 |
20040112594 | Aronstam | Jun 2004 | A1 |
20060193203 | Tenghamn et al. | Aug 2006 | A1 |
20080253226 | Tenghamn et al. | Oct 2008 | A1 |
20090147626 | Vahida et al. | Jun 2009 | A1 |
20090279387 | Tenghamn et al. | Nov 2009 | A1 |
20100118646 | Tenghamn | May 2010 | A1 |
20100118647 | Tenghamn | May 2010 | A1 |
20100322028 | Tenghamn | Dec 2010 | A1 |
20110038225 | Tenghamn | Feb 2011 | A1 |
20110069741 | Erickson | Mar 2011 | A1 |
20110075520 | Gulgne et al. | Mar 2011 | A1 |
20110085422 | Thompson et al. | Apr 2011 | A1 |
20110090759 | Laycock | Apr 2011 | A1 |
20110162906 | Harper | Jul 2011 | A1 |
20110297476 | Harper et al. | Dec 2011 | A1 |
20110317515 | Tenghamn | Dec 2011 | A1 |
20120075955 | Dean | Mar 2012 | A1 |
20120081997 | Babour et al. | Apr 2012 | A1 |
20120113747 | Ferber | May 2012 | A1 |
20120120759 | Le Page | May 2012 | A1 |
20120147699 | Dellinger et al. | Jun 2012 | A1 |
20120147709 | Zowarka, Jr. et al. | Jun 2012 | A1 |
20120155217 | Dellinger et al. | Jun 2012 | A1 |
20120188845 | Jeffryes | Jul 2012 | A1 |
20120232780 | Delson et al. | Sep 2012 | A1 |
20120271551 | Wei | Oct 2012 | A1 |
20120314536 | Bagaini | Dec 2012 | A1 |
20130037342 | Engdahl | Feb 2013 | A1 |
20130100777 | Ruet | Apr 2013 | A1 |
20130163386 | Sallas | Jun 2013 | A1 |
20140334254 | Zrostlik et al. | Nov 2014 | A1 |
20140334259 | Tenghamn | Nov 2014 | A1 |
20140340985 | Tenghamn et al. | Nov 2014 | A1 |
20150085605 | Tenghamn | Mar 2015 | A1 |
20150085606 | Tenghamn et al. | Mar 2015 | A1 |
20150085607 | Tenghamn | Mar 2015 | A1 |
20150085608 | Tenghamn et al. | Mar 2015 | A1 |
Number | Date | Country |
---|---|---|
1397142 | Mar 1965 | FR |
0071266 | Nov 2000 | WO |
2015063209 | May 2015 | WO |
2015063210 | May 2015 | WO |
2015063211 | May 2015 | WO |
Entry |
---|
“Synthesis of Design, Testing and Analysis Research on Steel Column Base Plate Connections in High-Seismic Zones”. Jorge E. Grauvilardell. D. Lee., J. F. Hajjar, RJ Dexter. Structural Engineering Report No. ST-04-02. Dept of Civil Eng. U of Minnesota. (2005) (Year: 2005). |
International Search Report and Written Opinion for App. No. PCT/CA2015/051262 dated Feb. 15, 2016. |
Hardee, H.C. et al: “Downhole Seismic Source”, Geophysics, vol. 52, No. 6, Jun. 1987, pp. 729-739. |
Feng et al., “A Class IV Flextensional Device Based on Electrostrictive Poly(vinylidene fluoride-trifluoroethylene,” Jun. 2003, pp. 1-6. |
Fons Ten Kroode et al., “Broadband seismic data—The importance of low frequencies,” Geophysics, Mar.-Apr. 2013, pp. WA3-WA14, vol. 78, No. 2. |
Rune Tenghamn, “PGS Electrical Marine Vibrator,” Tech Link, Nov. 2005, pp. 1-3, vol. 5, No. 11, Publication of PGS Geophysical. |
Rune Tenghamn and Andrew Long, “PGS shows off electrical marine vibrator to capture ‘alternative’ seismic source market,” First Break, Jan. 2006, pp. 11-14, vol. 24. |
Rune Tenghman, “Complementing Seismic Source Technology with Marine Vibrators,” Presented at PGS Technology day in Oslo, Norway, Oct. 16, 2012. |
Ralph S.Woollett, “Current Approaches to the Miniaturization and Pressure Release Problems of VLF Transducers,” Naval Underwater Systems Center, Nov. 5, 1973. |
Ralph S. Woollett, “Underwater Helmholtz-Resonator Transducers: General Design Principles,” NUSC Technical, Jul. 5, 1977. |
EP Search Report for Application No. 15865856.7 dated Jun. 19, 2018. |
EP Search Report for Application No. 15865856.7 dated Nov. 14, 2018. |
H.C. Hardee et al., Downhole Seismic Source, Geophysics, vol. 52, No. 6, Jun. 1, 1987. |
Number | Date | Country | |
---|---|---|---|
20160259078 A1 | Sep 2016 | US |
Number | Date | Country | |
---|---|---|---|
62086601 | Dec 2014 | US |