Page 163 - Reservoir Geomechanics
P. 163

146    Reservoir geomechanics


               Wellbore imaging


               Wellbore imaging devices make it possible to obtain direct information on the distribu-
               tion and orientation of fractures and faults encountered at depth. One family of wellbore
               image tools is collectively known as the ultrasonic borehole televiewer (BHTV). Such
               tools scan the wellbore wall with a centralized rotating ultrasonic (several hundred
               kilohertz to ∼1megahertz) transducer that is oriented with respect to magnetic north
               (Figure 5.3a from Zemanek, Glenn et al. 1970). The amplitude of the reflected pulse
               is diminished when the wellbore wall is rough (such as where a fracture or bedding
               plane intersects the well) and the travel time increases when the wellbore radius is
               enlarged by features such as wellbore breakouts (Chapter 6). These devices provide
               an image of both the acoustic reflectance and the radius of the wellbore such that it is
               possible to construct three-dimensional images of a wellbore (Figure 5.3b after Barton,
               Tessler et al. 1991). The reflectance depends on both the stiffness of the formation
               and the smoothness of the wellbore wall. Figure 5.3d illustrates an unwrapped image
               of the wellbore wall in which position around the well (with respect to north in this
               case) is shown on the abscissa and depth is shown on the ordinate. The amplitude of the
               reflected pulse is displayed as brightness. In such a display, planar fractures (or bedding
               planes) cutting the wellbore (Figure 5.3c) have a sinusoidal appearance (Figure 5.3d)
               resulting from the low amplitude of the reflected acoustic pulse along the intersection
               of the fault plane and wellbore wall. The dip direction is obvious in the unwrapped
               image (the direction of the lowest point where the fracture leaves the wellbore) and the
               amount of dip is determined from

                       −1
               Dip = tan (h/d)                                                    (5.5)

               where h is the height of the fracture as measured at the top and bottom of its intersection
               with the wellbore and d is the diameter of the well. In Chapter 6,we will demonstrate
               another important application of borehole televiewer data in the context of analysis
               of stress-induced compressional wellbore failures (or breakouts) as the time it takes
               the pulse to travel to/from the wellbore wall (and knowledge of the acoustic velocity
               of the wellbore fluid) enables one to reconstruct the detailed cross-sectional shape of
               the wellbore wall. Ultrasonic wellbore imaging is now available from a number of
               geophysical logging companies. While the details of operation of these types of instru-
               ments are slightly different (such as the number of pulses per rotation, the frequency of
               the ultrasonic transducer and the way in which the transducer beam is focused on the
               wellbore wall), the fundamental operation of all such tools is quite similar.
                 Figure5.4bisanunwrappedimageofwellborewallmadewiththeothertypeofimage
               data used widely in the oil and gas industry, an electrical imaging device that uses arrays
               of electrodes on pads mounted on arms that press against the wellbore wall. The imaging
               device (Figure 5.4a from Ekstrom, Dahan et al. 1987) monitors the contact resistance
   158   159   160   161   162   163   164   165   166   167   168