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220                                       Intelligent Digital Oil and Gas Fields


          where C D is the data covariance matrix. The relationship between the data
          and the model parameters is expressed as a nonlinear function that maps the
          model parameters into the data space, d5g[m], where d is the data vector
          with N observations representing the output of the model, m is a vector of
          size M whose elements are the model parameters, and g is the forward model
          operator, a function that relates the model parameters to the output. For
          history-matching problems, g represents the reservoir simulator.
             Using Bayes’ inference (Eq. 6.8), the posterior pdf can be defined as
          follows:
                               p m|d mj dÞ∝ exp  O m                  (6.11)
                                  ð
                                              ½
                                                  ðފ
          where O(m) represents the Bayesian OF in multi-Gaussian notation:
                    1          T   1             1       0 T   1       0

            O mðÞ ¼ ð d gmðÞÞ C ð    d gmðÞÞ +     m m      C M  m m
                                  d
                    2                            2
                                                                      (6.12)
          The first right-hand term of Eq. 6.12 represents the data misfit term (mis-
          match between observed data and simulated response), while the second
          right-hand term corresponds to a regularization term, usually represented
          by the prior/known geomodel. The result of minimizing the O(m) (Eq.
          6.12) is called the Maximum-A-Posteriori (MAP) estimate because it rep-
          resents the most likely posterior model. The set of parameters m that min-
          imizes O(m) is the most probable estimate.
             The goal of the Bayesian approach is to derive a statistical distribution
          for the model parameters via posterior distribution, constrained through
          the prior distribution. Because the reservoir history-matching problem is
          an inverse problem, its solution renders multiple plausible models (i.e.,
          multiple realizations), and the consequence of nonlinearity is that one
          must resort to an iterative solution. The MAP estimate is often insufficient
          because it does not provide the uncertainty quantification in the posterior
          model. As a solution, Kitanidis (1995) and Oliver et al. (1996) introduced
          the randomized maximum likelihood (RML) method which provides a
          theoretically rigorous approach to sample from the posterior distribution
          but holds only for linear Gaussian problems, which are seldom the case
          for reservoir simulation model inversion. Several alternative approaches
          for a rigorous sampling from posterior distribution for nonlinear problems
          have been proposed, such as traditional Markov chain Monte Carlo
          (McMC) (Neal, 1993), its multistage implementation with enhancements
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