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Analytical  Expressions of  the  Posterior  Operator  133

            Table 6.1. Examples of  parameters and operators in  Equation  6.17.

          Soft  Data
          Equation        B                      D                 5f
          3.32             I                     I        Xao/t   Eq.  6.1

          3.33             1                     I        ^(X»y* Eq.  6.3
          3.34        J R1 dFXC;  h)             J(0     Xso/t    Eq.  6.8
          3.35                                           Xso/t    Eq.  6.9

        COMMENT  6.2 : One should   keep   i n mind   that   th e posterior   operator   i n



        Equation 6.17   i s a   mathematical   quantity   representing   ou r  state  o f knowl-



        edge o f the physical phenomenon under study.  Consequently,  th e ^ -operator
        has epistemic   features  that   allow  it  to  possess whatever properties  the   mod-

        ern geo'statistician   chooses   based   on   available   knowledge,   the   goals   of   the


        study, etc. The only   requirements are that the corresponding  pdfmust  satisfy

        the mathematical  conditions  of  a pdf  and   that   the  results   of  any  calculations




        we make   with this pdf agree   with   the physical  data,   scientific   laws,  etc.
            The  above  results  certainly  do  not  exhaust all  possibilities  regarding  the
        ^-operators.  These results deal with knowledge that can be expressed in terms
        of  the  natural  variable X.  However,  knowledge that  depends on  some  other
        variables  Y\,  Y%,  etc.  can  also  be  studied  by  BME  (e.g.,  Chapter  9).  The
        reader  is encouraged to  consider  operators that  best  describe physical  knowl-
        edge about a scientific or engineering problem of his/her own interest and derive
        mathematical  expressions for  the  relevant  posterior  operator.  Certain  imple-
        mentations  of  the  BME  formulas  above could  be computationally  intensive,
        especially when multiple integrations  over pdf's are involved.  However, contin-
        uing  progress in  numerical  approximation  techniques  (Monte  Carlo,  etc.),  as
        well as the fast-developing  technology of workstations  and parallel computation
        is expected  to  handle such computational  issues  efficiently.
            The  derivation  of  the  BME  posterior  pdf  (Eq.  6.17)  does not  involve any
        of  the  restrictive  assumptions and approximations  used  by other  geostatistical
        methods,  such as the  multi-Gaussian and  indicator  approaches. Limitations  of
        the multi-Gaussian characterization of posterior probability  distributions  include
        (Goovaerts,  1997):  (a)  strong  assumptions are made about  the  multivariate
        probability  distribution,  which  usually cannot  be checked in  practice;  (b)  ex-
        tremely  large and  low values are considered spatially  uncorrelated, which  is of-
        ten  an invalid  assumption;  (c)  the  corresponding variance is data-independent.
        The  indicator  approach suffers from  theoretical  and  practical  limitations  such
        as  (Olea,  1999):  (i)  unfeasible values for cdf may be obtained; (ii) the  derived
        cdf  sometimes  fail  order-relationship  requirements;  (m)  the  large  number  of
        indicator  thresholds  involved  require heavy computational  and inference efforts
        (to  reduce these efforts  approximations are introduced,  which may make things
        worse);  (iv)  the  approach  can account  for  only a few cases of  imprecise  data;
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