Modern oil field operations demand a great quantity of information relating to the parameters and conditions encountered downhole. Because drillers and operators are forced to operate remotely from the underground formations and reservoirs they wish to exploit, their access to relevant information is limited. Consequently, there is a demand for tools that provide new types of information, more accurate information, or more efficient collection of information. Examples of the information that may be collected include characteristics of the earth formations traversed by the borehole, and data relating to the size and configuration of the borehole itself. This information is usually recorded and displayed in the form of a log, i.e. a graph of the measured parameter as a function of tool position or depth. The collection of information relating to conditions downhole, which commonly is referred to as “logging”, can be performed by several methods including wireline logging and “logging while drilling” (LWD).
In wireline logging, a probe or “sonde” is lowered into the borehole after some or all of the well has been drilled. The sonde hangs at the end of a long cable or “wireline” that provides mechanical support to the sonde and also provides an electrical connection between the sonde and electrical equipment located at the surface of the well. In accordance with existing logging techniques, various parameters of the earth's formations are measured and correlated with the position of the sonde in the borehole as the sonde is pulled uphole.
In LWD, the drilling assembly includes sensing instruments that measure various parameters as the formation is being penetrated, thereby enabling measurements of the formation while it is less affected by fluid invasion. While LWD measurements are desirable, drilling operations create an environment that is generally hostile to electronic instrumentation, telemetry, and sensor operations.
In these and other logging environments, it is desirable to construct an image of the borehole wall. Among other things, such images reveal the fine-scale structure of the penetrated formations. The fine-scale structure includes stratifications such as shale/sand sequences, fractures, and non-homogeneities caused by irregular cementation and variations in pore size. Orientations of fractures and strata can also be identified, enabling more accurate reservoir flow modeling.
Borehole wall imaging can be accomplished in a number of ways, but micro-resistivity tools have proven to be effective for this purpose. Micro-resistivity tools measure borehole surface resistivity on a fine scale. The resistivity measurements can be converted into pixel intensity values to obtain a borehole wall image. However, oil-based muds can inhibit such measurements due to the high resistivity of the mud and the variability of the contact impedance due to variable standoff. U.S. Pat. No. 6,191,588 (Chen) discloses an imaging tool for use in oil-based muds. Chen's resistivity tool employs at least two pairs of voltage electrodes positioned on a non-conductive surface between a current source electrode and a current return electrode. At least in theory, the separation of voltage and current electrodes eliminates the oil-based mud's effect on voltage electrode measurements, enabling at least qualitative measurements of formation resistivity.
In constructing an imaging tool for use in oil-based muds, certain engineering constraints on the structural strength of sensor pads will be recognized. These engineering constraints may be met by making the sensor pad base out of a metal such as steel. Though the steel can be insulated to present a non-conductive external surface, the electrical conductivity of the base creates potential current leakage paths. These leakage paths adversely affect the tool's resistivity measurements.
In the following detailed description, reference will be made to the accompanying drawings, in which:
The drawings show illustrative invention embodiments that will be described in detail. However, the description and accompanying drawings are not intended to limit the invention to the illustrative embodiments, but to the contrary, the intention is to disclose and protect all modifications, equivalents, and alternatives falling within the spirit and scope of the appended claims.
Disclosed herein are various leakage current compensation methods and systems for imaging in nonconductive fluids such as an oil-based mud. In some embodiments, disclosed logging systems include a logging tool in communication with surface computing facilities such as a personal computer, server, digital signal processing board, or some other form of computing circuit. The logging tool is provided with a sensor array having at least two voltage electrodes positioned between at least two current electrodes that create an electric field in a borehole wall, and is further provided with an electronic circuit to determine a differential voltage between the voltage electrodes in response to different source current frequencies from the current electrodes. The voltage measurements at different frequencies enable compensation for leakage current effects. From the voltage measurements at different frequencies, the computing facilities can determine compensated borehole wall resistivity as a function of depth and azimuth, and may display the resistivity as a borehole wall image.
A LWD resistivity imaging tool 26 is integrated into the bottom-hole assembly near the bit 14. As the bit extends the borehole through the formations, tool 26 collects measurements relating to various formation properties as well as the tool orientation and various other drilling conditions. The resistivity imaging tool 26 may take the form of a drill collar, i.e., a thick-walled tubular that provides weight and rigidity to aid the drilling process. A telemetry sub 28 may be included to transfer tool measurements to a surface receiver 30 and to receive commands from the surface.
At various times during the drilling process, the drill string 8 may be removed from the borehole as shown in
The mudcake and fluid flow layers have a very low conductivity, which creates some difficulty for high-resolution measurements of borehole wall resistivity. The mudcake creates additional problems where low resistivity formations are measured, because the current flow into the formation may be relatively small and in turn generates an extremely small voltage difference that is difficult to measure. Measurements through the low-conductivity layers may be improved by: (1) using an alternating current; (2) separating the voltage electrodes in order to increase the signal (at the cost of degrading spatial resolution); and (3) using a source current with a higher operating frequency.
A cross-section of the illustrative sensor pad 502 is shown in
In some embodiments, metal substrate 602 comprises steel. The face of metal substrate 602 is covered with an insulating layer 606, which in some embodiments comprises a polyetheretherketone (PEEK) material. Current electrodes 506 and 508 are embedded on the face of the insulating layer 606. Shields 510 and 512 separate the current electrodes 506 and 508 from the body of pad 502, and the lines that feed current electrodes 506, 508 are preferably also shielded, possibly with the line shields in a coaxial cable or triaxial cable configuration. In some embodiments, shields are also provided for the voltage electrodes and voltage electrode feeds. Separating the current electrodes from the electrode shields are insulating inserts 608, which in some embodiments comprise a PEEK material.
At higher measurement frequencies, capacitive coupling to the metal substrate creates leakage currents. Such leakage currents can severely impair resistivity measurements. To enable measurements at such frequencies, the geometric design of the pad should be tailored to minimize capacitive coupling (e.g., by increasing the thickness of the insulating materials). Moreover the use of guard electrodes, particularly when combined with a current sensing design that excludes current flow from the guard electrodes, is particularly effective at minimizing the effects of current leakage. Nevertheless, some residual leakage currents may be expected
Measurement circuitry 902 comprises a current or voltage source 906 that drives an oscillating current between the current electrodes. A current sensor may be coupled to the current electrodes to measure total current flow between the electrodes. Measurement circuitry 902 further includes a detector 916 for each voltage electrode pair to measure the potential difference generated by the formation currents. Detector 916 may take the form of a differential voltage amplifier, and in alternative embodiments, may take the form of separate sense amplifiers for each voltage electrode. In both cases, circuitry 902 may include analog-to-digital converters to enable digital processing of the measured potential differences. These potential differences are associated with a position on the borehole wall and processed to estimate formation resistivity at that position.
Equivalent circuit 904 includes components 920-924 that approximate theoretical current paths between the current electrodes. Capacitor 920 represents a current path through the body of pad 502, whereas resistor 922 and capacitor 924 represent current paths passing through the formation. The current labeled IL flows through capacitor 920, and the current labeled IF flows through resistor 922 and capacitor 924. The total source current is IT=IL+IF. More sophisticated equivalent circuit models are contemplated and may be used. Each equivalent circuit should include at least one component to represent formation impedance and at least one component to represent leakage impedance.
In equivalent circuit 904, the impedance of the two current paths varies differently as a function of frequency. It can be shown that
where R is the formation resistance (represented by resistor 922), CF is the formation capacitance (represented by capacitor 924), and CL is the leakage capacitance (represented by capacitor 920). Thus the equation for the total impedance has three unknowns. If the total impedance is measured at n frequencies and separated into real (in-phase) and imaginary (quadrature phase) components, there are 2 n equations from which the unknowns can be determined.
For example, let the total impedances measured at two different frequencies be:
then it can be shown with some algebraic manipulation after equating with equation (1) that:
Expressions for CL and CF can also be written out. The formation resistance can be accurately obtained. If it is desired to determine the measurement current IF, the leakage current can be calculated:
and subtracted from the total current. In this manner the phase and amplitude of the measurement current are obtained. For more sophisticated equivalent circuit models having more unknowns, measurements at additional frequencies can be used to calculate the formation resistivity and any other unknowns of interest. More sophisticated equivalent circuit models often have better accuracy in describing the physical problem.
In block 1304, the tool is placed in logging mode. For LWD, this operation may (or may not) involve deploying a de-centralizer that forces sensors in the tool body against the borehole wall. Alternatively, the LWD resistivity imaging tool may have one or more sensor pads that are deployed against the borehole wall. For wireline logging, multiple sensor pads are deployed against the borehole wall.
Blocks 1306-1316 represent operations that occur during the logging process. Though shown and described in a sequential fashion, the various operations may occur concurrently, and moreover, they may simultaneously occur for multiple voltage electrode pairs and multiple sensor pads. In block 1306, the source driving the current electrodes begins operating at a first frequency, and a first differential voltage measurement is made between the voltage electrodes. In block 1308, the source driving the current electrodes operates at a second frequency and a second differential voltage measurement is made between the voltage electrodes. In other embodiments, the current signal provides power at multiple frequencies simultaneously, which can be done with a sum of sinusoidal signal of different frequencies (i.e., a combination of narrowband signals), or with a wideband signal such as white noise or a signal that resembles an impulse in the time domain. As the tool energizes the formation via the current electrodes, the tool measures the amplitude and relative phase of the differential voltages between the various voltage electrode pairs. For the simultaneous multi-frequency embodiments, the differential voltage measurements may be filtered or transformed to obtain the amplitude and phase response for each frequency.
From the current and differential voltage measurements, the total impedance at each frequency is determined in block 1310 and may be used to determine a leakage current and/or to directly determine a formation resistivity. If the formation resistivity is not directly determined in block 1310, then in block 1312, a measurement current and formation resistivity may be determined based in part on the leakage current. Also in block 1312, the tool, or more likely, the surface logging facility coupled to the tool, associates the compensated resistivity measurements with a tool position and orientation measurement, thereby enabling a determination of borehole wall image pixel values.
In block 1314, the tool moves along the borehole, and in block 1316, a check is performed to determine whether logging operations should continue (e.g., whether the logging tool has reached the end of the region of interest). For continued logging operations, blocks 1306-1316 are repeated. Once logging operations are complete, the surface logging facility maps the resistivity measurements into borehole wall image pixels and displays a resistivity image of the borehole wall in block 1318. Alternatively, the resistivity image may be displayed as it is being created during logging operations.
A variety of voltage electrode geometries are possible and may be used. A greater number of voltage electrodes may provide higher resolution at the expense of increased processing costs. The operating voltages and currents may vary widely while remaining suitable for the logging operations described herein. It has been found that source current frequencies above about 5 kHz, and perhaps as high as 100 kHz or more, are desirable as they reduce the mud layer impedances and increase the voltage differences measurable between the voltage electrodes. Higher frequencies generally provide larger measurement signals, but they also increase leakage currents, making the compensation methods disclosed herein even more desirable. In some tool embodiments, the source current frequency may be switchable between low frequency regions (e.g., around 10 kHz) and high frequency regions (e.g., around 80 kHz) for measurements in formations of differing resistivity. Higher frequencies may be preferred for formations having a generally lower resistivity, and vice versa.
While illustrative embodiments of this invention have been shown and described, modifications thereof can be made by one skilled in the art without departing from the spirit or teaching of this invention. The embodiments described herein are illustrative and are not limiting. Many variations and modifications of the system and apparatus are possible and are within the scope of the invention. For example, though the disclosure and claims use the term “resistivity”, it is widely recognized that conductivity (the inverse of resistivity) has a one-to-one correspondence with resistivity and, consequently, often serves as a functional equivalent to resistivity. Accordingly, the scope of protection is not limited to the embodiments described herein, but is only limited by the claims which follow, the scope of which shall include all equivalents of the subject matter of the claims.
The present application claims priority to U.S. Provisional Patent Application 60/749,765, filed Dec. 13, 2005 and entitled “Multiple Frequency Based Leakage Current Correction For Imaging In Oil-Based Muds”, which is hereby incorporated herein by reference.
Filing Document | Filing Date | Country | Kind | 371c Date |
---|---|---|---|---|
PCT/US2006/061860 | 12/11/2006 | WO | 00 | 3/25/2008 |
Publishing Document | Publishing Date | Country | Kind |
---|---|---|---|
WO2007/070777 | 6/21/2007 | WO | A |
Number | Name | Date | Kind |
---|---|---|---|
3086195 | Halliday | Apr 1963 | A |
3305771 | Arps | Feb 1967 | A |
3462678 | Eaton | Aug 1969 | A |
3470457 | Howlett | Sep 1969 | A |
3973181 | Calvert | Aug 1976 | A |
4012952 | Dory | Mar 1977 | A |
4072923 | Siems et al. | Feb 1978 | A |
4241611 | Specht et al. | Dec 1980 | A |
4361808 | Kern et al. | Nov 1982 | A |
4468623 | Gianzero et al. | Aug 1984 | A |
4532615 | Ballinger | Jul 1985 | A |
4567759 | Ekstrom et al. | Feb 1986 | A |
4677367 | Goodman | Jun 1987 | A |
4692707 | Locke et al. | Sep 1987 | A |
4718011 | Patterson | Jan 1988 | A |
5044462 | Maki | Sep 1991 | A |
5144126 | Perry et al. | Sep 1992 | A |
5160925 | Dailey et al. | Nov 1992 | A |
5216242 | Perry et al. | Jun 1993 | A |
5235285 | Clark et al. | Aug 1993 | A |
5251708 | Perry et al. | Oct 1993 | A |
5278550 | Rhein-Knudson et al. | Jan 1994 | A |
5331318 | Montgomery | Jul 1994 | A |
5339037 | Bonner | Aug 1994 | A |
5359180 | Park et al. | Oct 1994 | A |
5396175 | Seeman | Mar 1995 | A |
5570024 | Vail et al. | Oct 1996 | A |
5596534 | Manning | Jan 1997 | A |
5691712 | Meek et al. | Nov 1997 | A |
5992223 | Sabins et al. | Nov 1999 | A |
6023168 | Minerbo | Feb 2000 | A |
6173793 | Thompson et al. | Jan 2001 | B1 |
6191588 | Chen | Feb 2001 | B1 |
6252518 | Laborde | Jun 2001 | B1 |
6268726 | Prammer et al. | Jul 2001 | B1 |
6332109 | Sheard et al. | Dec 2001 | B1 |
6348796 | Evans et al. | Feb 2002 | B2 |
6362619 | Prammer et al. | Mar 2002 | B2 |
6373254 | Dion et al. | Apr 2002 | B1 |
6396276 | Van Steenwyk et al. | May 2002 | B1 |
6518756 | Morys et al. | Feb 2003 | B1 |
6564883 | Fredericks et al. | May 2003 | B2 |
6583621 | Prammer et al. | Jun 2003 | B2 |
6600321 | Evans | Jul 2003 | B2 |
6603314 | Kostelnicek et al. | Aug 2003 | B1 |
6626251 | Sullivan et al. | Sep 2003 | B1 |
6636406 | Anthony | Oct 2003 | B1 |
6688396 | Floerke et al. | Feb 2004 | B2 |
6714014 | Evans et al. | Mar 2004 | B2 |
6717501 | Hall et al. | Apr 2004 | B2 |
6809521 | Tabarovsky et al. | Oct 2004 | B2 |
6815930 | Goodman | Nov 2004 | B2 |
6825659 | Prammer et al. | Nov 2004 | B2 |
6850068 | Chemali et al. | Feb 2005 | B2 |
6891377 | Cheung et al. | May 2005 | B2 |
6975112 | Morys et al. | Dec 2005 | B2 |
7109719 | Fabris et al. | Sep 2006 | B2 |
7119544 | Hayman et al. | Oct 2006 | B2 |
7139218 | Hall et al. | Nov 2006 | B2 |
7145472 | Lilly et al. | Dec 2006 | B2 |
7154412 | Dodge et al. | Dec 2006 | B2 |
7207396 | Hall et al. | Apr 2007 | B2 |
7242194 | Hayman et al. | Jul 2007 | B2 |
7463027 | Prammer et al. | Dec 2008 | B2 |
7579841 | San Martin et al. | Aug 2009 | B2 |
7696756 | Morys et al. | Apr 2010 | B2 |
7733086 | Prammer et al. | Jun 2010 | B2 |
7888941 | San Martin et al. | Feb 2011 | B2 |
20020043369 | Vinegar et al. | Apr 2002 | A1 |
20020153897 | Evans et al. | Oct 2002 | A1 |
20030155925 | Tabarovsky et al. | Aug 2003 | A1 |
20030173968 | Cheung et al. | Sep 2003 | A1 |
20030222651 | Tabanou | Dec 2003 | A1 |
20040124837 | Prammer et al. | Jul 2004 | A1 |
20040245991 | Hayman et al. | Dec 2004 | A1 |
20050067190 | Tabanou | Mar 2005 | A1 |
20050133262 | Chen et al. | Jun 2005 | A1 |
20050179437 | Hayman et al. | Aug 2005 | A1 |
20070046291 | Itskovich | Mar 2007 | A1 |
20070103161 | San Martin et al. | May 2007 | A1 |
20090309591 | Goodman et al. | Dec 2009 | A1 |
Number | Date | Country |
---|---|---|
105801 | Apr 1984 | EP |
1035299 | Sep 2000 | EP |
2289340 | Nov 1995 | GB |
2391070 | Jan 2004 | GB |
2401185 | Mar 2004 | GB |
WO2005059285 | Jun 2005 | WO |
Number | Date | Country | |
---|---|---|---|
20080252296 A1 | Oct 2008 | US |
Number | Date | Country | |
---|---|---|---|
60749765 | Dec 2005 | US |