Abstract:
The present disclosure relates to a method to determine the vertical resistivity of a subsurface formation. A downhole logging tool having a plurality of spaced antennas, at least one of which is a transverse antenna, at least two of which are tilted antennas, and at least two of which are axial antennas is provided. Measurements involving the transverse and/or the tilted antennas of the downhole logging tool are obtained. Voltage ratios are formed using the measurements, and conditioning factors are formed by raising the determined voltage ratios not involving the transverse antenna to some arbitrary power. The sum of the exponents of the conditioning factors preferably equals one. A voltage ratio involving the transverse antenna is multiplied by the conditioning factors, and the vertical resistivity of the subsurface formation is determined using the resulting ratio.

Description:
CROSS-REFERENCE TO OTHER APPLICATIONS 
     N/A 
     BACKGROUND 
     1. Technical Field 
     The present disclosure relates generally to the logging of subsurface formations surrounding a wellbore using a downhole logging tool, and particularly to using the logs to estimate the anisotropic resistivity. 
     2. Background Art 
     Logging tools have long been used in wellbores to make, for example, formation evaluation measurements to infer properties of the formations surrounding the borehole and the fluids in the formations. Common logging tools include electromagnetic tools, nuclear tools, and nuclear magnetic resonance (NMR) tools, though various other tool types are also used. 
     Early logging tools were run into a wellbore on a wireline cable, after the wellbore had been drilled. Modern versions of such wireline tools are still used extensively. However, the need for information while drilling the borehole gave rise to measurement-while-drilling (MWD) tools and logging-while-drilling (LWD) tools. MWD tools typically provide drilling parameter information such as weight on the bit, torque, temperature, pressure, direction, and inclination. LWD tools typically provide formation evaluation measurements such as resistivity, porosity, and NMR distributions (e.g., T1 and T2). MWD and LWD tools often have components common to wireline tools (e.g., transmitting and receiving antennas), but MWD and LWD tools must be constructed to not only endure but to operate in the harsh environment of drilling. 
     Certain existing resistivity logging tools have at least one transverse antenna. That is, the magnetic dipole moment of the transverse antenna is perpendicular to the longitudinal axis of the tool. For example, one model of the Schlumberger Technology Corporation&#39;s PERISCOPE™ logging tools measures the propagation of electromagnetic signals with an array of transmitter and receiver coils that includes two tilted receivers and one transverse transmitter. The tool obtains directional information, and also detects anisotropic resistivity. 
     SUMMARY 
     The present disclosure relates to a method to determine the vertical resistivity of a subsurface formation. A downhole logging tool is provided having a plurality of spaced antennas, at least one of which is a transverse antenna, at least two of which are tilted antennas, and at least two of which are axial antennas. Measurements of the transverse-to-tilted, and tilted-to-axial couplings are obtained. When the relative dip angle is small, only measurements of transverse-to-tilted couplings are sensitive to resistivity anisotropy. They may be combined with measurements of tilted-to-axial couplings, to achieve several objectives: (1) improve relative sensitivity to anisotropy; (2) improve vertical response; and (3) avoid the need to calibrate the antennas individually. 
     Other aspects and advantages will become apparent from the following description and the attached claims. 
    
    
     
       BRIEF DESCRIPTION OF THE FIGURES 
         FIG. 1  illustrates an exemplary well site system. 
         FIG. 2  shows a prior art electromagnetic logging tool. 
         FIG. 3  is a schematic drawing of a particular resistivity logging tool that may be used in accordance with the present disclosure. 
         FIG. 4  is a plot showing the behavior of the ratio             at 400 kHz in a homogeneous medium at zero dip, assuming point dipole coils, in accordance with the present disclosure.
         FIG. 5  is a plot showing the behavior of the ratio 1/            at 400 kHz in a homogeneous medium at zero dip, assuming point dipole coils, in accordance with the present disclosure.
         FIG. 6  is a set of plots showing the simulation results of the ratio             in a model formation for frequencies of 100 kHz and 400 kHz, in accordance with the present disclosure.
         FIG. 7  is a set of plots showing the simulation results of the ratio             in a model formation for frequencies of 100 kHz and 400 kHz, in accordance with the present disclosure.
     
    
    
     DETAILED DESCRIPTION 
     Some embodiments will now be described with reference to the figures. Like elements in the various figures will be referenced with like numbers for consistency. In the following description, numerous details are set forth to provide an understanding of various embodiments and/or features. However, it will be understood by those skilled in the art that some embodiments may be practiced without many of these details and that numerous variations or modifications from the described embodiments are possible. As used here, the terms “above” and “below”, “up” and “down”, “upper” and “lower”, “upwardly” and “downwardly”, and other like terms indicating relative positions above or below a given point or element are used in this description to more clearly describe certain embodiments. However, when applied to equipment and methods for use in wells that are deviated or horizontal, such terms may refer to a left to right, right to left, or diagonal relationship as appropriate. 
       FIG. 1  illustrates a well site system in which various embodiments can be employed. The well site can be onshore or offshore. In this exemplary system, a borehole  11  is formed in subsurface formations by rotary drilling in a manner that is well known. Some embodiments can also use directional drilling, as will be described hereinafter. 
     A drill string  12  is suspended within the borehole  11  and has a bottom hole assembly  100  which includes a drill bit  105  at its lower end. The surface system includes platform and derrick assembly  10  positioned over the borehole  11 , the assembly  10  including a rotary table  16 , kelly  17 , hook  18  and rotary swivel  19 . The drill string  12  is rotated by the rotary table  16 , energized by means not shown, which engages the kelly  17  at the upper end of the drill string. The drill string  12  is suspended from a hook  18 , attached to a traveling block (also not shown), through the kelly  17  and a rotary swivel  19  which permits rotation of the drill string relative to the hook. As is well known, a top drive system could alternatively be used. 
     In the example of this embodiment, the surface system further includes drilling fluid or mud  26  stored in a pit  27  formed at the well site. A pump  29  delivers the drilling fluid  26  to the interior of the drill string  12  via a port in the swivel  19 , causing the drilling fluid to flow downwardly through the drill string  12  as indicated by the directional arrow  8 . The drilling fluid exits the drill string  12  via ports in the drill bit  105 , and then circulates upwardly through the annulus region between the outside of the drill string and the wall of the borehole, as indicated by the directional arrows  9 . In this well known manner, the drilling fluid lubricates the drill bit  105  and carries formation cuttings up to the surface as it is returned to the pit  27  for recirculation. 
     The bottom hole assembly  100  of the illustrated embodiment includes a logging-while-drilling (LWD) module  120 , a measuring-while-drilling (MWD) module  130 , a roto-steerable system and motor, and drill bit  105 . 
     The LWD module  120  is housed in a special type of drill collar, as is known in the art, and can contain one or a plurality of known types of logging tools. It will also be understood that more than one LWD and/or MWD module can be employed, e.g. as represented at  120 A. (References, throughout, to a module at the position of  120  can alternatively mean a module at the position of  120 A as well.) The LWD module includes capabilities for measuring, processing, and storing information, as well as for communicating with the surface equipment. In the present embodiment, the LWD module includes a resistivity measuring device. 
     The MWD module  130  is also housed in a special type of drill collar, as is known in the art, and can contain one or more devices for measuring characteristics of the drill string and drill bit. The MWD tool further includes an apparatus (not shown) for generating electrical power to the downhole system. This may typically include a mud turbine generator powered by the flow of the drilling fluid, it being understood that other power and/or battery systems may be employed. In the present embodiment, the MWD module includes one or more of the following types of measuring devices: a weight-on-bit measuring device, a torque measuring device, a vibration measuring device, a shock measuring device, a stick/slip measuring device, a direction measuring device, and an inclination measuring device. 
     An example of a tool which can be the LWD tool  120 , or can be a part of an LWD tool suite  120 A, is shown in  FIG. 2 . 
     Recent electromagnetic logging tools use one or more tilted or transverse antennas, with or without axial antennas. Those antennas may be transmitters or receivers. A tilted antenna is one whose dipole moment is neither parallel nor perpendicular to the longitudinal axis of the tool. A transverse antenna is one whose dipole moment is perpendicular to the longitudinal axis of the tool, and an axial antenna is one whose dipole moment is parallel to the longitudinal axis of the tool. Two antennas are said to have equal angles if their dipole moment vectors intersect the tool&#39;s longitudinal axis at the same angle. For example, two tilted antennas have the same tilt angle if their dipole moment vectors, having their tails conceptually fixed to a point on the tool&#39;s longitudinal axis, lie on the surface of a right circular cone centered on the tool&#39;s longitudinal axis and having its vertex at that reference point. Transverse antennas obviously have equal angles of 90 degrees, and that is true regardless of their azimuthal orientations relative to the tool. 
     Resistivity logging tools having certain combinations of tilted and transverse antennas can be used to obtain better logs of the vertical resistivity, R v , in anisotropic formations. In particular, data involving the transverse antenna can be combined into a computed quantity that provides an improved estimate of R v . For ease of discussion, a particular resistivity logging tool is shown in  FIG. 3 . The nomenclature for the transmitters (T) and the receivers (R) is shown in  FIG. 3 . The nominal axial positions of the coils are listed in Table 1.  FIG. 3  also shows the relative spacings for various transmitter/receiver pairs. 
     
       
         
               
               
               
             
               
               
               
             
           
               
                   
                 TABLE 1 
               
               
                   
                   
               
               
                   
                 Coil 
                 Axial position (inches) 
               
               
                   
                   
               
             
             
               
                   
               
             
          
           
               
                   
                 R3 
                 −62 
               
               
                   
                 T5 
                 −40 
               
               
                   
                 T3 
                 −28 
               
               
                   
                 T1 
                 −16 
               
               
                   
                 R1 
                 −3 
               
               
                   
                 R2 
                 3 
               
               
                   
                 T6 
                 12 
               
               
                   
                 T2 
                 22 
               
               
                   
                 T4 
                 34 
               
               
                   
                 R4 
                 56 
               
               
                   
                   
               
             
          
         
       
     
     The following ratio is known to be sensitive to the anisotropy R v /R h : 
                     ℛ     A   ⁢           ⁢   59   ⁢   o       =         〈     T   ⁢           ⁢   6   ⁢   R   ⁢           ⁢   3     〉       〈     T   ⁢           ⁢   6   ⁢   R   ⁢           ⁢   4     〉       .             Eq   .           ⁢   0               
In the subscript “A 59o ”, “A” stands for the anisotropy measurement, and “59” (inches) corresponds to the average of the T6R3 (74 inches) and T6R4 (44 inches) spacings, as in the example given in Table 1. It should be understood that for another layout of transmitters and receivers this average spacing may be different, and that the discussion below is general and by no means restricted to or by the specific average spacing of 59 inches being considered in this example. The angle brackets indicate averages over the tool rotation angle. The ratio             involves the complex (phasor) voltage recorded at two different receivers produced by the same transmitter current, each voltage averaged over the rotation of the tool. The term “voltage ratio” will be used herein for this type of signal combination. Note that the ratio           is sensitive to calibrations (shifts in the attenuation and the phase) of both tilted receivers R3 and R4, and it would be desirable to compensate for this dependence.

     At present, one manner in which the information from transmitter T6 in the representative tool is processed is as the ratio: 
                     ℛ     A   ⁢           ⁢   59   ⁢   a       =         〈     T   ⁢           ⁢   6   ⁢   R   ⁢           ⁢   3     〉       〈     T   ⁢           ⁢   6   ⁢   R   ⁢           ⁢   4     〉       ⁢         〈     T   ⁢           ⁢   2   ⁢   R   ⁢           ⁢   4     〉       〈     T   ⁢           ⁢   2   ⁢   R   ⁢           ⁢   3     〉       .               Eq   .           ⁢   1               
This ratio can be thought of as comprising two voltage ratios, one voltage ratio involving the transverse antenna and one voltage ratio not involving the transverse antenna. For small dip angles (i.e., near-vertical wells), the ratio R A59a  is relatively insensitive to the vertical conductivity, σ v , particularly in resistive formations.
 
     An alternative ratio that could be used is: 
     
       
         
           
             
               
                 
                   
                     ℛ 
                     
                       A 
                       ⁢ 
                       
                           
                       
                       ⁢ 
                       59 
                       ⁢ 
                       b 
                     
                   
                   = 
                   
                     
                       
                         〈 
                         
                           T 
                           ⁢ 
                           
                               
                           
                           ⁢ 
                           6 
                           ⁢ 
                           R 
                           ⁢ 
                           
                               
                           
                           ⁢ 
                           3 
                         
                         〉 
                       
                       
                         〈 
                         
                           T 
                           ⁢ 
                           
                               
                           
                           ⁢ 
                           6 
                           ⁢ 
                           R 
                           ⁢ 
                           
                               
                           
                           ⁢ 
                           4 
                         
                         〉 
                       
                     
                     ⁢ 
                     
                       
                         
                           〈 
                           
                             T 
                             ⁢ 
                             
                                 
                             
                             ⁢ 
                             3 
                             ⁢ 
                             R 
                             ⁢ 
                             
                                 
                             
                             ⁢ 
                             4 
                           
                           〉 
                         
                         
                           〈 
                           
                             T 
                             ⁢ 
                             
                                 
                             
                             ⁢ 
                             3 
                             ⁢ 
                             R 
                             ⁢ 
                             
                                 
                             
                             ⁢ 
                             3 
                           
                           〉 
                         
                       
                       . 
                     
                   
                 
               
               
                 
                   Eq 
                   . 
                   
                       
                   
                   ⁢ 
                   2 
                 
               
             
           
         
       
     
     To enhance the sensitivity to σ v , we consider a generalization of the form: 
                     ℛ     A   ⁢           ⁢   59   ⁢   c       =         〈     T   ⁢           ⁢   6   ⁢   R   ⁢           ⁢   3     〉       〈     T   ⁢           ⁢   6   ⁢   R   ⁢           ⁢   4     〉       ⁢       (       〈     T   ⁢           ⁢   2   ⁢   R   ⁢           ⁢   4     〉       〈     T   ⁢           ⁢   2   ⁢   R   ⁢           ⁢   3     〉       )       1   2       ⁢         (       〈     T   ⁢           ⁢   3   ⁢   R   ⁢           ⁢   4     〉       〈     T   ⁢           ⁢   3   ⁢   R   ⁢           ⁢   3     〉       )       1   2       .               Eq   .           ⁢   3               
Unlike            , the ratios          ,          , and           in Eqs. 1, 2, and 3 do not require coil calibration. If there is a change in the magnetic moment of one of the coils, or if its phase is shifted, the ratio          , for example, remains unchanged. Also, the ratio           is not affected by a change in the current in one of the transmitters or the gain in one of the receiver amplifiers. Similarly, the ratios           and           are not affected by these changes. The attenuation decrement (dB) and phase shift (degrees) that correspond to each ratio is obtained from:

                     atten   =     20   ⁢       log   10     ⁡     (     abs   ⁡     (   ℛ   )       )           ,     phase   =       -     180   π       ⁢       angle   ⁡     (   ℛ   )       .                 Eq   .           ⁢   4               
In Eq. 4,             denotes one of the ratios defined above (         ,          , or          ). As in all LWD resistivity measurements, an appropriate air calibration correction is needed before inversion.

     In  FIG. 3 , it is seen that T2R4 and T3R3 have the same spacing (34 inches). Also T2R3 and T3R4 have the same spacing (84 inches). Therefore, in a homogeneous medium we have, theoretically, 
                         〈     T   ⁢           ⁢   2   ⁢   R   ⁢           ⁢   4     〉       〈     T   ⁢           ⁢   2   ⁢   R   ⁢           ⁢   3     〉       ⁢       〈     T   ⁢           ⁢   3   ⁢   R   ⁢           ⁢   4     〉       〈     T   ⁢           ⁢   3   ⁢   R   ⁢           ⁢   3     〉         =   1.           Eq   .           ⁢   5               
This relation is also valid in any medium with no z variation, where z denotes position along the tool axis. Further, it is also valid if the medium is symmetric about the plane z=−3 inches.
 
     As an alternative to Eq. 3, the following ratio could be used: 
                     ℛ     A   ⁢           ⁢   59   ⁢   d       =         〈     T   ⁢           ⁢   6   ⁢   R   ⁢           ⁢   3     〉       〈     T   ⁢           ⁢   6   ⁢   R   ⁢           ⁢   4     〉       ⁢       (       〈     T   ⁢           ⁢   4   ⁢   R   ⁢           ⁢   4     〉       〈     T   ⁢           ⁢   4   ⁢   R   ⁢           ⁢   3     〉       )       1   2       ⁢         (       〈     T   ⁢           ⁢   5   ⁢   R   ⁢           ⁢   4     〉       〈     T   ⁢           ⁢   5   ⁢   R   ⁢           ⁢   3     〉       )       1   2       .               Eq   .           ⁢   6               
T4R4 and T5R3 have the same spacing (22 inches), as seen in  FIG. 3 . Also T4R3 and T5R4 have the same spacing (96 inches). Theoretically, in a homogeneous medium, we expect that:
 
     
       
         
           
             
               
                 
                   
                     
                       
                         〈 
                         
                           T 
                           ⁢ 
                           
                               
                           
                           ⁢ 
                           4 
                           ⁢ 
                           R 
                           ⁢ 
                           
                               
                           
                           ⁢ 
                           4 
                         
                         〉 
                       
                       
                         〈 
                         
                           T 
                           ⁢ 
                           
                               
                           
                           ⁢ 
                           4 
                           ⁢ 
                           R 
                           ⁢ 
                           
                               
                           
                           ⁢ 
                           3 
                         
                         〉 
                       
                     
                     ⁢ 
                     
                       
                         〈 
                         
                           T 
                           ⁢ 
                           
                               
                           
                           ⁢ 
                           5 
                           ⁢ 
                           R 
                           ⁢ 
                           
                               
                           
                           ⁢ 
                           4 
                         
                         〉 
                       
                       
                         〈 
                         
                           T 
                           ⁢ 
                           
                               
                           
                           ⁢ 
                           5 
                           ⁢ 
                           R 
                           ⁢ 
                           
                               
                           
                           ⁢ 
                           3 
                         
                         〉 
                       
                     
                   
                   = 
                   1. 
                 
               
               
                 
                   Eq 
                   . 
                   
                       
                   
                   ⁢ 
                   7 
                 
               
             
           
         
       
     
     A more general ratio that does not require coil calibration is: 
                       ℛ     A   ⁢           ⁢   59   ⁢   e       =         〈     T   ⁢           ⁢   6   ⁢   R   ⁢           ⁢   3     〉       〈     T   ⁢           ⁢   6   ⁢   R   ⁢           ⁢   4     〉       ⁢       (       〈     T   ⁢           ⁢   1   ⁢   R   ⁢           ⁢   4     〉       〈     T   ⁢           ⁢   1   ⁢   R   ⁢           ⁢   3     〉       )     α     ⁢       (       〈     T   ⁢           ⁢   2   ⁢   R   ⁢           ⁢   4     〉       〈     T   ⁢           ⁢   2   ⁢   R   ⁢           ⁢   3     〉       )     β     ⁢       (       〈     T   ⁢           ⁢   3   ⁢   R   ⁢           ⁢   4     〉       〈     T   ⁢           ⁢   3   ⁢   R   ⁢           ⁢   3     〉       )     γ     ⁢       (       〈     T   ⁢           ⁢   4   ⁢   R   ⁢           ⁢   4     〉       〈     T   ⁢           ⁢   4   ⁢   R   ⁢           ⁢   3     〉       )     δ     ⁢       (       〈     T   ⁢           ⁢   5   ⁢   R   ⁢           ⁢   4     〉       〈     T   ⁢           ⁢   5   ⁢   R   ⁢           ⁢   3     〉       )       1   -   α   -   β   -   γ   -   δ           ,           Eq   .           ⁢   8               
where α, β, γ, and δ are arbitrary real numbers. The voltage ratios that are expressly raised to some power (i.e., those not involving a transverse antenna) are referred to herein as “conditioning factors”.             reduces to           when α=δ=0 and β=γ=½. Use of the ratio           is generally preferable.

     The behavior of             in a homogeneous medium is plotted in  FIG. 4 . The dip angle is zero and the frequency is 400 kHz. The response was computed from the Moran-Gianzero formulas that assume point-dipole coils. [J. H. Moran and S. Gianzero, Effects of formation anisotropy on resistivity-logging measurements,  Geophysics  44, 1266-1286 (1979)]. The corresponding information for           is plotted in  FIG. 5 . For convenience,  FIG. 5  gives the attenuation and phase of the reciprocal ratio 1/         . In a homogeneous medium, at low conductivity, the leading term in           is proportional to σ v , whereas           gets a strong contribution from σ h  that masks the more subtle σ v  dependence.
     If σ v  varies while σ h  is held fixed, the absolute change in atten and phase is the same in  FIGS. 4 and 5 . At zero dip angle, terms like            T2R3)          are independent of σ v  because the coupling between axial coils is not affected by anisotropy. However,  FIG. 5  is more advantageous because of the greater relative change in atten and phase. Also, in  FIG. 5 , changes in σ v  are more easily distinguished from changes in σ h .
     To understand the vertical response of these measurements, simulated logs were computed for the model formation with a step profile. The relative dip angle is zero. The values of R h  (horizontal resistivity) and R v  increase by steps, as shown in the left panel of  FIG. 6 . The values of R h  are 10 (upper four sublayers), 20 (middle four sublayers), and 50 ohm-m (lower four sublayers). For each respective sublayer within each of those three four-sublayer blocks, the ratio R v /R h  has the values 1, 2, 5, and 10. 
     The simulated logs were computed with a semi-analytic code for a medium with transversely isotropic parallel plane layers with dip. The computed attenuation and phase shift logs are shown in  FIGS. 6 and 7 . They assume point dipole coils. The results for the A 59a  computation are plotted in the second and third panels of  FIG. 6 . The dashed-line curves in each of those plot panels (one for attenuation, one for phase shift) correspond to a 400 kHz signal. The solid-line curve in each of those plot panels corresponds to the ratio             computed for a frequency of 100 kHz.
     The second and third plot panels of  FIG. 7  display the computed logs for the A 59c  ratio. The dashed-line curves in the attenuation (second) plot panel and the phase shift (third) plot panel corresponds to the 400 kHz signal. The solid-line curves correspond to the 100 kHz signal in the attenuation plot panel and the phase shift plot panel. 
     Changes in R v  produce a bigger relative change in the phase and attenuation for the ratio            , as compared to those for           in  FIG. 6 . Also, the location of the bed boundaries is more easily inferred from these logs than from the logs of  FIG. 6 . After inversion, the ratio           yields a better estimate of the vertical resistivity R v  than the           ratio.
     It should be appreciated that while the invention has been described with respect to a limited number of embodiments, those skilled in the art, having benefit of this disclosure, will appreciate that other embodiments can be devised which do not depart from the scope of the invention as disclosed herein. Accordingly, the scope of the invention should be limited only by the attached claims.