WO2010068883A2 - Multi-frequency borehole imager - Google Patents
Multi-frequency borehole imager Download PDFInfo
- Publication number
- WO2010068883A2 WO2010068883A2 PCT/US2009/067696 US2009067696W WO2010068883A2 WO 2010068883 A2 WO2010068883 A2 WO 2010068883A2 US 2009067696 W US2009067696 W US 2009067696W WO 2010068883 A2 WO2010068883 A2 WO 2010068883A2
- Authority
- WO
- WIPO (PCT)
- Prior art keywords
- acoustic waves
- frequency
- new
- earth formation
- transducer
- Prior art date
- Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
- Ceased
Links
Classifications
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/40—Seismology; Seismic or acoustic prospecting or detecting specially adapted for well-logging
- G01V1/44—Seismology; Seismic or acoustic prospecting or detecting specially adapted for well-logging using generators and receivers in the same well
- G01V1/46—Data acquisition
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/003—Seismic data acquisition in general, e.g. survey design
- G01V1/006—Seismic data acquisition in general, e.g. survey design generating single signals by using more than one generator, e.g. beam steering or focusing arrays
Definitions
- the invention disclosed herein relates to imaging an earth formation from a borehole using acoustic waves.
- Well logging is a technique used to perform measurements of an earth formation from a borehole penetrating the formation.
- a logging instrument is conveyed through the borehole.
- the logging instrument performs the measurements of the formation through the borehole.
- a wireline is used to support the logging instrument and to transmit measurements to the surface of the earth for processing and recording.
- acoustic waves travel from the instrument through a fluid in the borehole and into the earth formation.
- the earth formation in turn reflects some of the acoustic waves back to the instrument where the waves are recorded.
- the intensity of acoustic waves reflected from a part of the formation is related to the material composing that particular part of the formation.
- the acoustic image can provide a visual indication of the various materials present in the formation.
- acoustic images having higher accuracy or higher resolution require acoustic waves with a higher frequency.
- the frequency of the acoustic waves increase, the more attenuation of the acoustic waves by the borehole fluid occurs.
- Attenuation of acoustic waves causes weaker reflective waves and, therefore, a weaker acoustic measurement signal.
- the weaker measurement signal can result in a decrease in accuracy or resolution of the image.
- resolution of an acoustic image of an earth formation is limited by the attenuating characteristics of the borehole fluid.
- the techniques can be used in a borehole containing a fluid.
- an apparatus for imaging an earth formation including: a logging instrument configured to be conveyed through a borehole penetrating the earth formation; a source of acoustic waves disposed at the logging instrument, wherein the source is configured to emit first acoustic waves having at least a first frequency and to enable intermodulation of the first acoustic waves in a medium having a nonlinear acoustic property resulting in generating new acoustic waves that are transmitted to the earth formation, the new acoustic waves having a new frequency different from the at least first frequency; and a receiver of acoustic waves configured to receive the new acoustic waves reflected from the earth formation, wherein the received new acoustic waves provide an image of the earth formation.
- Also disclosed is a method for imaging an earth formation including: conveying a logging instrument through a borehole penetrating the earth formation; emitting first acoustic waves from the logging instrument, the first acoustic waves comprising at least a first frequency and directed to the earth formation; generating new acoustic waves by intermodulation of the first acoustic waves in a nonlinear acoustic medium wherein the new acoustic waves have a new frequency different from the at least first frequency and are transmitted into the earth formation; and receiving the new acoustic waves that are reflected by the earth formation, wherein the received new acoustic waves provide an image of the earth formation.
- a machine-readable medium having machine-executable instructions for imaging an earth formation by implementing the following steps: emitting first acoustic waves from a logging instrument disposed in a borehole penetrating the earth formation, the first acoustic waves having at least a first frequency and directed to the earth formation; generating new acoustic waves by intermodulation of the first acoustic waves in a nonlinear acoustic medium wherein the new acoustic waves have a new frequency different from the at least first frequency and are transmitted into the earth formation; and receiving the new acoustic waves that are reflected by the earth formation, wherein the received new acoustic waves provide an image of the earth formation.
- FIG. 1 illustrates an exemplary embodiment of a logging instrument disposed in a borehole penetrating an earth formation
- FIG. 2 depicts aspects of an embodiment of a source of acoustic waves having two confocal acoustic transducers
- FIG. 3 depicts aspects an embodiment of the source of acoustic waves having one acoustic transducer
- FIGS. 4A and 4B collectively referred to as FIG. 4, depict aspects of an embodiment of the source of acoustic waves having a receiver disposed between two acoustic transducers;
- FIG. 5 presents one example of a method for imaging an earth formation.
- the techniques which include apparatus and method, call for transmitting acoustic waves from a logging instrument through a borehole penetrating the earth formation.
- the logging instrument is configured to transmit the acoustic waves such that the acoustic waves experience intermodulation within a fluid disposed in the borehole.
- the intermodulation causes the transmitted acoustic waves to generate new acoustic waves at a higher frequency than any of the acoustic waves transmitted by the logging instrument. Because the new acoustic waves are generated closer to a wall of the borehole, there is less attenuation of the higher frequency new acoustic waves. Less attenuation of the higher frequency new acoustic waves results in an acoustic image having increased accuracy and resolution.
- intermodulation relates to acoustic waves (referred to hereinafter as first acoustic waves) interacting with each other to generate new acoustic waves having a frequency different from the first acoustic waves.
- the interaction generally occurs in a medium, such as a borehole fluid, having a nonlinear acoustic property. If the first acoustic waves have a frequency fl and a frequency f2, then the new acoustic waves can have a sum frequency acoustic wave fl+f2 and a difference frequency acoustic wave fl-f2.
- the new sum frequency acoustic wave can provide an acoustic image with increased resolution.
- overlap relates to the first acoustic waves occupying substantially the same space at the same time with the same phase as required for intermodulation of the first acoustic waves.
- FIG. 1 there is shown a depiction of an instrument 10 for performing acoustic imaging.
- the instrument (or acoustic tool) 10 is disposed within a borehole 2 penetrating earth formation 3.
- the instrument 10 includes a source 4 of first acoustic waves 5.
- the first acoustic waves 5 travel through a borehole fluid 9 in the borehole 2 where the first acoustic waves 5 experience intermodulation.
- new acoustic waves 6 of a higher frequency are generated.
- the new acoustic waves 6 enter the formation 3.
- the formation 3 reflects at least a portion of the new acoustic waves 6 back to the instrument 10.
- a receiver 7 receives the reflected new acoustic waves 6 and converts the energy of reflected new acoustic waves 6 into a signal 8.
- the signal 8 can be recorded and/or processed by an electronic unit 11.
- Stored data in the electronic unit 11 can be retrieved when the instrument 10 is removed from the borehole 2.
- the signal 8 can be transmitted by a telemetry system to the surface of the earth and received by a processing system 12 for recording and processing, hi addition, the electronic unit 11 can be used to control/operate the source 4.
- Non-limiting examples of control functions of the electronic unit 11 include modulating the amplitude of the first acoustic waves 5, varying a frequency of the first acoustic waves 5, and varying a phase of the first acoustic waves 5. These control functions can be used to enable and/or optimize the intermodulation of the first acoustic waves 5.
- the borehole 2 is at least partially filled with a mixture of liquids including water, drilling fluid, mud, oil and formation fluids that are indigenous to the formations 3 penetrated by the borehole 2.
- Drilling mud may also be introduced into the borehole 2.
- the drilling mud is a non-conductive or conductive fluid as is known in the art.
- the fluid 9 disposed in the borehole 2 generally has a nonlinear acoustic property that enables intermodulation of the first acoustic waves 5.
- the logging instrument 10 is supported by a wireline 13.
- the wireline 13 is also used to transmit data (i.e., the signal 8) related to acoustic imaging measurements performed by the logging instrument 10.
- the logging instrument 10 can be conveyed through the borehole 2 by slickline, coiled tubing, or a drill string for logging-while-drilling (LWD) measurements.
- LWD logging-while-drilling
- the logging instrument 10 may be disposed in a collar attached to the drill string.
- FIG. 2 depicts aspects of one embodiment of the source 4 for the first acoustic waves 5.
- a single transducer body 20 includes a first acoustic transducer 21 concentric or confocal with a second acoustic transducer 22.
- the first acoustic transducer 21 emits first acoustic waves 5 with frequency fl and the second acoustic transducer 22 emits first acoustic waves 5 of frequency f2.
- the first acoustic transducer 21 and the second acoustic transducer 22 are configured to provide sufficient overlap to enable intermodulation of the first acoustic waves at substantially the wall of the borehole 2. Because of the intermodulation, the new acoustic waves 6 are generated with frequencies fl+f2 and fl-f2. In the embodiment of FIG. 2, the frequencies fl and £2 are slightly different.
- the new acoustic waves 6 of frequencies fl and fl enter the formation 3.
- some amount of the new acoustic waves 6 will be reflected back towards the instrument 10 (not shown) to be received by the receiver 7 (not shown) and converted to the signal 8 (not shown).
- the receiver 7, the electronic unit 11, or the processing system 12 can be configured to filter out the new acoustic waves 6 of frequency fl-f2.
- the waves of frequency fl+f2 can be filtered out to produce an acoustic image made from waves of frequency fl-f2.
- the two images can then be compared to determine more information about the formation 3.
- the receiver 7 can be optimized for any of the resulting frequencies of the new acoustic waves 6 that are to be analyzed.
- FIG. 3 depicts aspects of another embodiment of the source 4.
- the first transducer 21 is used to emit the first acoustic waves 5.
- the amplitude of the first acoustic waves 5 is highly modulated, generally at very high input voltages. Because of a nonlinear property of the borehole fluid 9, the first acoustic waves 5 will undergo intermodulation and generate the new acoustic waves 6 at sum and difference frequencies. The amount of amplitude modulation can be varied to determine an optimal amount for causing intermodulation.
- the electronic unit 11 is used to modulate the amplitude of the first acoustic waves 5.
- FIG. 4 (4A is a top view and 4B is a three-dimensional side view) depicts aspects of yet another embodiment of the source 4.
- the receiver 7 is disposed between the first acoustic transducer 21 and the second acoustic transducer 22.
- the first acoustic transducer 21 emits the first acoustic waves 5 having frequency fl and the second acoustic transducer 22 emits the first acoustic waves 5 having frequency f2.
- the first acoustic transducer 21 and the second acoustic transducer 22 are positioned so that the first acoustic waves 5 emitted from the transducers 21 and 22 converge substantially at the wall of the borehole 2.
- the positions of the first acoustic transducer 21 and the second acoustic transducer 22 are configured to produce sufficient overlap to enable intermodulation of the first acoustic waves 5.
- the intermodulation of the first acoustic waves 5 having frequencies fl and f2 generate the new acoustic waves 6 having sum frequency fl +f2 and difference frequency fl-f2.
- the receiver 7 is positioned to receive the new acoustic waves 6 that are reflected by materials in the formation 3.
- the logging instrument 10 can be used with the following three methods for imaging the formation 3 around the borehole 2.
- the imaging can be for 360 degrees or any arc selected.
- a part of the instrument 10 supporting the source 4 of the first acoustic waves 5 and the receiver 7 is rotated around the borehole 2.
- an array of source 4 sets, such as those shown in FIGS. 2, 3 and 4, each with an associated receiver 7 can be disposed around the logging instrument 10 to provide 360 degrees of coverage.
- the new acoustic waves 6 generated by the intermodulation of first acoustic waves 5 from each source 4 meet adjacent new acoustic waves 6 to provide continuous imaging.
- a third method is similar to the second method but uses an array with a smaller number of the source 4/receiver 7 sets.
- a beam of the new acoustic waves 6 is electronically or mechanically steered (by the electronic unit 11 for example) around the borehole 2 to provide the 360-degree or selected arc coverage.
- electronic steering can include applying more power to one of two acoustic transducers in the source 4, thereby tilting a beam of the first acoustic waves 5 more in the direction of the transducer with the higher power output.
- mechanical steering can include the source 4 being mounted on a servo- controlled gimbal, thereby electromechanically varying a direction of a beam of the first acoustic waves 5 and, thus, varying a direction of a beam of the new acoustic waves 6.
- Use of intermodulation to generate the new acoustic waves 6 at the sum frequency can improve azimuthal resolution by a factor of about two.
- Amplitude and time-of-flight analysis of the new acoustic waves 6 reflected by the formation 3 can be used to provide information about the formation 3.
- processing the reflected new acoustic waves 6 can be performed in the frequency domain using a Fourier Transform or Wavelet analysis.
- the sum frequency (fl+f2) of the new acoustic waves 6 is a result of the sum of the frequencies of the first acoustic waves 5 or an amount of amplitude modulation, a user can control the frequencies of the first acoustic waves 5 or the amount of amplitude modulation to vary the sum frequency of the new acoustic waves 6. Varying the sum frequency of the new acoustic waves 6 can be particularly useful for various types and sizes of borehole features in different drilling muds.
- FIG. 5 presents one example of a method 50 for imaging the earth formation 3.
- the method 50 calls for (step 51) conveying the logging instrument 10 through the borehole 2 penetrating the earth formation 3. Further, the method 50 calls for (step 52) emitting the first acoustic waves 5 from the logging instrument 10, the first acoustic waves 5 having at least a first frequency and directed to the earth formation 3. Further, the method 50 calls for (step 53) generating the new acoustic waves 6 by intermodulation of the first acoustic waves 5 in the nonlinear acoustic medium 9 wherein the new acoustic waves 6 have a new frequency different from the at least first frequency and are transmitted into the earth formation 3. Further, the method 50 calls for (step 54) receiving the new acoustic waves 6 that are reflected by the earth formation 3, wherein the received new acoustic waves 6 provide an image of the earth formation 3.
- various analysis components may be used, including a digital and/or an analog system.
- the electronic unit 11 and the processing system 12 can include the digital and/or analog system.
- the system may have components such as a processor, storage media, memory, input, output, communications link (wired, wireless, pulsed mud, optical or other), user interfaces, software programs, signal processors (digital or analog) and other such components (such as resistors, capacitors, inductors and others) to provide for operation and analyses of the apparatus and methods disclosed herein in any of several manners well-appreciated in the art.
- a power supply e.g., at least one of a generator, a remote supply and a battery
- cooling component heating component
- motive force such as a translational force, propulsional force or a rotational force
- magnet electromagnet
- sensor electrode
- transmitter receiver
- transceiver antenna
- controller optical unit
- electrical unit or electromechanical unit may be included in support of the various aspects discussed herein or in support of other functions beyond this disclosure.
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- Life Sciences & Earth Sciences (AREA)
- Physics & Mathematics (AREA)
- Remote Sensing (AREA)
- Engineering & Computer Science (AREA)
- Acoustics & Sound (AREA)
- Geology (AREA)
- Environmental & Geological Engineering (AREA)
- General Life Sciences & Earth Sciences (AREA)
- General Physics & Mathematics (AREA)
- Geophysics (AREA)
- Geophysics And Detection Of Objects (AREA)
- Measuring Or Testing Involving Enzymes Or Micro-Organisms (AREA)
- Measurement Of Velocity Or Position Using Acoustic Or Ultrasonic Waves (AREA)
Abstract
Description
Claims
Priority Applications (3)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| GB1109661.7A GB2477482B (en) | 2008-12-12 | 2009-12-11 | Multi-frequency borehole imager |
| BRPI0923367A BRPI0923367B1 (en) | 2008-12-12 | 2009-12-11 | apparatus and method for image formation of a terrestrial formation |
| NO20110833A NO343366B1 (en) | 2008-12-12 | 2011-06-08 | Multi-frequency logging instrument and method for mapping the subsurface around a borehole |
Applications Claiming Priority (4)
| Application Number | Priority Date | Filing Date | Title |
|---|---|---|---|
| US12194408P | 2008-12-12 | 2008-12-12 | |
| US61/121,944 | 2008-12-12 | ||
| US12/635,108 | 2009-12-10 | ||
| US12/635,108 US8559268B2 (en) | 2008-12-12 | 2009-12-10 | Multi-frequency borehole imager |
Publications (3)
| Publication Number | Publication Date |
|---|---|
| WO2010068883A2 true WO2010068883A2 (en) | 2010-06-17 |
| WO2010068883A3 WO2010068883A3 (en) | 2010-09-10 |
| WO2010068883A4 WO2010068883A4 (en) | 2010-11-11 |
Family
ID=42240343
Family Applications (1)
| Application Number | Title | Priority Date | Filing Date |
|---|---|---|---|
| PCT/US2009/067696 Ceased WO2010068883A2 (en) | 2008-12-12 | 2009-12-11 | Multi-frequency borehole imager |
Country Status (5)
| Country | Link |
|---|---|
| US (1) | US8559268B2 (en) |
| BR (1) | BRPI0923367B1 (en) |
| GB (1) | GB2477482B (en) |
| NO (1) | NO343366B1 (en) |
| WO (1) | WO2010068883A2 (en) |
Families Citing this family (4)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| US10094945B2 (en) * | 2014-03-24 | 2018-10-09 | Baker Hughes, A Ge Company, Llc | Formation measurements using nonlinear guided waves |
| GB2531792B (en) * | 2014-10-31 | 2020-08-12 | Bae Systems Plc | Communication system |
| GB2531793A (en) | 2014-10-31 | 2016-05-04 | Bae Systems Plc | Communication apparatus |
| GB2531795B (en) | 2014-10-31 | 2018-12-19 | Bae Systems Plc | Communication system |
Family Cites Families (13)
| Publication number | Priority date | Publication date | Assignee | Title |
|---|---|---|---|---|
| US4102185A (en) * | 1976-12-09 | 1978-07-25 | Texaco Inc. | Acoustic-nuclear permeability logging system |
| SU913303A1 (en) | 1978-07-25 | 1982-03-15 | Volzh Otdel I Geol Razrabotki | METHOD OF ACOUSTIC CARRIAGE AND DEVICE FOR ITS IMPLEMENTATION 1 |
| US5521882A (en) * | 1993-11-19 | 1996-05-28 | Schlumberger Technology Corporation | Measurement of formation characteristics using acoustic borehole tool having sources of different frequencies |
| US5535751A (en) * | 1994-12-22 | 1996-07-16 | Morphometrix Technologies Inc. | Confocal ultrasonic imaging system |
| SE9601387D0 (en) * | 1996-04-12 | 1996-04-12 | Siemens Elema Ab | Device for monitoring measuring electrodes for recording physiological measurement signals and their leads |
| US5780784A (en) * | 1996-10-17 | 1998-07-14 | Halliburton Energy Services, Inc. | Cancellation of tool mode signal from combined signal |
| US6775388B1 (en) * | 1998-07-16 | 2004-08-10 | Massachusetts Institute Of Technology | Ultrasonic transducers |
| US6440075B1 (en) * | 2000-10-02 | 2002-08-27 | Koninklijke Philips Electronics N.V. | Ultrasonic diagnostic imaging of nonlinearly intermodulated and harmonic frequency components |
| US7301852B2 (en) * | 2003-08-13 | 2007-11-27 | Baker Hughes Incorporated | Methods of generating directional low frequency acoustic signals and reflected signal detection enhancements for seismic while drilling applications |
| US7088639B2 (en) * | 2004-11-17 | 2006-08-08 | Rdsp I L.P. | Method for determining formation quality factor from well log data and its application to seismic reservoir characterization |
| US7319639B2 (en) * | 2004-12-20 | 2008-01-15 | Luna Innovations Incorporated | Acoustic concealed item detector |
| US8116167B2 (en) * | 2008-06-12 | 2012-02-14 | Chevron U.S.A. Inc. | Method and system for generating a beam of acoustic energy from a borehole, and applications thereof |
| US7839718B2 (en) * | 2008-07-02 | 2010-11-23 | Chevron U.S.A. Inc. | Device and method for generating a beam of acoustic energy from a borehole, and applications thereof |
-
2009
- 2009-12-10 US US12/635,108 patent/US8559268B2/en active Active
- 2009-12-11 WO PCT/US2009/067696 patent/WO2010068883A2/en not_active Ceased
- 2009-12-11 BR BRPI0923367A patent/BRPI0923367B1/en active IP Right Grant
- 2009-12-11 GB GB1109661.7A patent/GB2477482B/en active Active
-
2011
- 2011-06-08 NO NO20110833A patent/NO343366B1/en unknown
Also Published As
| Publication number | Publication date |
|---|---|
| WO2010068883A3 (en) | 2010-09-10 |
| NO343366B1 (en) | 2019-02-11 |
| WO2010068883A4 (en) | 2010-11-11 |
| GB201109661D0 (en) | 2011-07-27 |
| NO20110833A1 (en) | 2011-07-01 |
| BRPI0923367B1 (en) | 2020-01-21 |
| GB2477482A (en) | 2011-08-03 |
| US8559268B2 (en) | 2013-10-15 |
| BRPI0923367A2 (en) | 2015-07-21 |
| GB2477482B (en) | 2013-07-24 |
| US20100149914A1 (en) | 2010-06-17 |
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