Page 131 - Statistics and Data Analysis in Geology
P. 131

Statistics and Data Analysis in  Geology - Chapter 5

             As n becomes infinitely large, all of the fractions that contain n in their denominator
             become infinitesimally small and vanish, so all terms inside parentheses  simply
             become equal to 1. The terms inside the brackets simplify to

                                          P (r) = e  (-AA)                         (5.12)
                                                         r!
             Note that n, the number of  drilling sites, has vanished from the equation leaving
             only the discovery-well density, A, the number of  discovery wells, Y, and the area,
             A, of the tracts. This is an expression of  the Poisson distribution, as applied to the
             probability  of  rare, random events (discovery wells) occurring within geographic
              areas. Also note that AA is simply the mean number of wells per tract, because it is
             the product of  the density of  discovery wells times the area of  a tract. In practice,
             we estimate AA  from the total number of  discovery wells, m, and the total number
              of  tracts, T                          m
                                               hA=-                                 (5.13)
                                                     T
                 We  can now perform a x2 test to see if the number of  wells per tract matches
              that expected if  the wells are randomly located  according to the Poisson model.
             The number of  tracts that contain exactly r discovery wells can be found by

                                              nr = mP(r)
                                                 = me  (-hA)                        (5.14)
                                                            r!
             If AA is estimated by m/T, the equation becomes

                                                                                    (5.15)
              Figure 5-6  shows the locations of  discovery wells in part of  the Eastern Shelf area
              of  the Permian Basin in Fisher and Noland counties of  Texas.  The area has been
              divided into a lox 16 grid of 160 tracts, or quadrats, each containing approximately
              10 mi2. Since there are 168 discovery wells in the area, the mean number of  wells
             per tract is
                                            m    168
                                            -=-      = 1.05
                                            T    160
                 We  can count the number of  tracts in the map that contain no discovery wells,
              exactly one discovery, two discoveries, and so forth. Using Equation (5.15), we can
              also calculate the expected number of  tracts that contain these same numbers of
              wells. The expected and observed numbers of tracts for the Permian Basin area are
              given in Table  5-2.  This table contains all of  the figures necessary to calculate a
              x2 test of  goodness of  fit, which is essentially a comparison of  the two histograms
              shown in Figure 5-7.  The last three categories must be combined so that the ob-
              served number of  tracts is equal to or greater than five

                                   70 - 56.0)’   (42 - 58.8)’  + (26 - 30.9)’
                              2   J           +
                                -     56.0          58.8          30.9
                                   +  (17 - 10.8)’  + (5 - 3.5)2  = 13.28
                                         10.8         3.5
              ‘The test statistic has c - 2 degrees of freedom, where c is the number of  categories
              (one degree of  freedom is lost because the expected frequencies are constrained



              304
   126   127   128   129   130   131   132   133   134   135   136