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CPS1428 Enobong F. U.
                                  (  )
                            
                          ( + 1) (  )  − 1   
                   =  (               )⁄   (  )
                                  (  )    
                            
                          ( + 1) (  )  − 1  
                       ( )
                   =       
                          
                       ( + 1)
                  α=

                                                        x a

                                                                                         lnR(x b )

                                                                                        (e Q +1) lnR(x a ) ‐1
                                                                                   ln
                           lnR(x b )                 lnR(x m )            lnR(x b )       lnR(x b )

                                                               x b
                                           x b
                                                 Q
                        Q
                                                                      Q
                  ‐ {ln [(e +1) lnR(x a ) ‐1] ln ( x m )‐ln ( ) ln [(e +1) lnR(x a ) ‐1] +ln ( ) ln [(e +1) lnR(x a ) ‐1]} e { [(e Q +1) lnR(x a ) ‐1] }
                                                                                 ⁄
                                     x b   x a                 x a

                  where Q is the root of
                                         
                                                                              
                            (  ) ( +1)        (  ) ( +1)
                   (  ) −  (  (  )  − 1)  (  ) +  (  )  (  (  )  − 1) −
                                                      
                                     
                         (  ) ( +1)
                   (  )  (  (  )  − 1) = 0
                      
                      Observe that the only variable in equation (13) is x, which can easily be
                  obtained using appropriate iterative technique. Given the solution of equation
                  (13), values of c, k, and α are easily computed using equations (10), (11), and
                  (12) respectively. The values of c, k, and α can then be used to compute exact
                  values for activity mean and variance using equations (4) and (5). However, we
                  need the values of xa, xm, xb, with their corresponding probabilities F(xa) or R(xa)
                  , F(xm) or R(xm) and F(xb) or R(xb) for the computation of ,  and . These
                  quantities can be supplied by the expert as judgmental estimates or chosen
                  by the project manager based on apriori information.
                      One of the advantages of using the classical quantile technique to estimate
                  the parameters of Burr XII distribution is that the user has the liberty to choose
                  whatever quantile(s) he feels are appropriate. However, there is need to be
                  guided by the fact that the assessments of extreme quantiles like 0.0 and 1.0,
                  0.01 and 0.99 are difficult and almost unrealistic, since these extremes has to
                  do with the rare events. Quantiles like 0.10 and 0.90, 0.05 and 0.95 are found
                  to be more reliable and easy to assess, Moder et. al. (1983).
                      Some well known probability distributions that have been used as input
                  distributions in stochastic risk analysis are special cases of Burr XII distribution.
                  Table  I  presents  these  distributions  in  comparison  with  a  2P-Burr  XII

                  distribution.  Moreover,  Burr  XII  also  have  a  defined  mode  at    =
                                       1
                  [(  −  1) ⁄ (  +  1)]  ,if  > 1. Tadikamalla (1980)  have demonstrated that
                  Burr(XII) can fit a wide range of empirical data because it possesses a broad
                  range of skewness and kurtosis. Particularly, Burr (XII) region covers sections

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