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112      Modern Spatiotemporal   Geostatistics —  Chapter 5


             The conceptual and technical  issues introduced in the  preceding discussion
         are  best  clarified  with  the  help of  a few  simple examples.  Complex  situations
        can  be studied  as extensions of  the  simple, well-understood  solutions  to  these
        examples.  Frequent  references to  Chapter 3 are made in the following examples.

         EXAMPLE 5.3:  Consider the empirical law of  Example 3.6 (p. 77) which relates
         standard  penetration  resistance X  and vertical  stress Y  for a cohesionless soil.
         In  light  of  constraints  (Eqs.  3.8 and 3.9),  a  ^-based  prior  pdf  is given  by






        where
        the  subscripts a  and a'  account for  all  points  considered.  Other  constraints
        involving  the  multivariate  pdf  may  also  be  imposed.  Equation  5.16  is  sub-
        stituted  into  the  BME  equations  (Eqs.  3.8 and 3.9)  which  together  with  the
        normalization  constraint  can be solved for the  Lagrange multipliers  /ZQ, ^ a and
        /W-   This  process will  give  us the  ^-based  prior  pdf f s.  Note  that  it  is not
        necessary to  calculate the  cross covariance  between the  penetration  resistance
        and the vertical stress which  is,  nevertheless, taken into consideration implicitly
        in the  BME  equations above.

        EXAMPLE   5.4:  Let  us study  the  physical  law  expressed  by  Equation  3.16  (p.
        79).  From  the  set  of  equations  in  Equation  3.17  we  obtain  the  system  of
        moment  equations  below







        where the subscript  a  =  1,..., m,k  accounts for all times t a of interest.  In
        light of  Equation  5.17  and taking ho(t a)  =~go(t a)  =  1 into consideration, the
        9^-operator  in  Equation  5.7  is given  by






        From  Equation  5.17  we can write  in terms of the  pdf







        with  / ?(Xma P;  tmap)  =  exp [/i 0 +  %}•  By substituting  Equation  5.18  into
        Equation  5.19,  we get
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