Page 206 - Hydrocarbon Exploration and Production Second Edition
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Field Appraisal                                                       193


                                     well 1   well 2











                             dip angle                             fault
                              15 deg.
                                                     OWC




             Figure 8.2  Partially appraised structure.



                It should be noted that the RF for a reservoir is highly dependent on the
             development plan, and that initial conditions alone cannot be used to determine this
             parameter.
                In determining an estimate of reserves for an accumulation, all of the
             above parameters will be used. When constructing an expectation curve for
             STOIIP, GIIP or UR, a range of values for each input parameter should be used, as
             discussed in Section 7.2, Chapter 7. In determining an appraisal plan, it is necessary
             to determine which of the parameters contributes most to the uncertainty in
             STOIIP, GIIP or UR.
                Take an example of estimating GRV, based on seismic data and the results of two
             wells in a structure (Figure 8.2). The cross-section has been generated, and a base
             case GRV has been calculated.
                The general list of factors influencing the uncertainty in the GRV included the
             shape of structure, dip of flanks, position of bounding faults, position of internal
             faults and depth of fluid contacts (in this case the OWC). In the above example,
             the OWC is penetrated by two wells, and the dip of the structure can be
             determined from the measurements made in the wells, which in turn will allow
             calibration of the 3D seismic. The most significant sources of uncertainty in GRV
             are probably the position and dip of the bounding fault, and the extent of the
             field in the plane perpendicular to this section. By looking at the quality of the
             seismic data, an estimate may be made of the uncertainty in the position of
             the fault, and any indications of internal faulting which may affect the
             volumetrics. The determination of geological uncertainties requires knowledge
             of the environment of deposition, diagenesis and the structural pattern of the
             field. The quantification often starts with a subjective estimate based on regional
             knowledge of the geology. In cases where little data is available, ‘guesstimates’ may
             need to be supplemented with data or reservoir trends observed in neighbouring
             fields.
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