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Well Deviation, Surveying, and Geosteering  195

               west of true north in the Northern Hemisphere and east of true north in
               the Southern Hemisphere. Likewise, vertical grid lines to the east of the
               central meridian will point east of true north in the Northern Hemi-
               sphere and west of true north in the Southern Hemisphere. The so-called
               grid correction (G) is positive when TN is east of grid north, and nega-
               tive when it is west. Typical values are -1.5 to +1.5 degrees.
            •  True north. This is the direction of the geographic north pole as defined
               by the axis of rotation of the Earth. The meridians, or lines of longi-
               tude, on maps point toward true north.

                                   13.2 SURVEYING


               Borehole position uncertainty defines the range of actual possible posi-
            tions of a particular point in a well in terms of eastings, northings, and
            TVD. Factors that affect borehole position uncertainty are:

            1. Accuracy of measured depth determination in the well. Both
               drillpipe and wireline cable suffer from stretch and inaccuracies in the
               methods used to measure how much pipe or cable has been run into
               the hole. This uncertainty becomes greater with increasing depth and
               well deviation. For a vertical well drilled to 3,500m, one would expect
               the measured depth at total depth (TD) to be known to an accuracy of
               roughly 2m. For a deviated well drilled to 3,500m TVD with a devia-
               tion at bottom of 50 degrees, this inaccuracy might rise to 5m.
            2. Frequency of survey stations. When surveying a well, it is normal to
               acquire “stations” at discrete depth intervals along the well. At each of
               these stations, the hole’s inclination and azimuth will be measured.
               Between stations, it is necessary to use an algorithm to determine
               values to be interpolated. The accuracy of the final survey will depend
               on the frequency of these stations and algorithm used.
            3. Survey tool accuracy. Let us consider these different types of tools
               separately:
               (a) Magnetic survey tools. The accuracy of magnetic devices is limited
                   by their intrinsic accuracy and the extent to which they are affected
                   by magnetic interference. The strength and direction of the Earth’s
                   field is also a factor, since in a worst-case scenario of drilling in
                   the same direction as the Earth’s lines of flux, no azimuthal mea-
                   surement would be possible. Near the poles, the Earth’s field is
                   nearly vertical and this would be a factor. Magnetic interference
                   may come from any metal in proximity to the tool (such as the
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