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RESERVOIR COMPACTION, SUBSIDENCE AND WELL DAMAGE 345
            prevented from flowing (i.e., if the stress state is undrained). Alternatively, if the
            pore pressure is increased or decreased, then the effective stress on the volume of
            rock will change depending on the boundary conditions applied to the rock.
              For large deformation, elastoplastic analysis of compaction, the complete set of
            governing  equations  defines  a  transient  nonlinear  system,  which  must  be
            integrated numerically in the time domain. The system of equations is difficult to
            solve even for small problems, but especially difficult for large problems, such
            as  a  large-scale  reservoir  compaction  simulation.  The  theory  and  numerical
            solution of the nonlinear, completely coupled system by finite element methods
            has  been  presented  by  a  number  of  authors  for  applications  in  geotechnical
            engineering (i.e., consolidation and liquefaction) and petroleum engineering (i.e.,
            compaction). 55–57,86–88
              Though  the  fully  coupled  problem  is  highly  nonlinear,  some  general
            observations regarding the effects of coupling can be stated. The state of stress in
            the  reservoir  rock  under  compacting  conditions  is  compression.  The  weight  of
            the  overburden  is  the  mechanism  responsible  for  the  compression,  and  hence
            drives  the  compaction.  Compaction,  which  is  in  part  the  reduction  in  pore
            volume,  drives  fluid  from  the  pores,  or  causes  an  increase  of  the  pore  fluid
            pressure, if the fluid is prevented from flowing. By the same token, the stress is
            affected by the pore pressure change, which affects the overall stress state in and
            around the reservoir, and hence affects the amount of compaction. Both of these
            effects are the salient effects of the coupling between rock deformations and pore
            fluid pressure. Historically, it has been the case that most reservoir flow simulators
            have no geomechanical capability, and therefore do not include coupling. That
            is, the rock matrix is incompressible, though the fluid may be compressible and
            multiphase.  In  such  simulators,  measured  volumes  of  oil,  water  and  gas,
            produced or injected, are “history matched” to the wells and reservoir pressure
            behavior computed with the simulator. The resulting pressure fields are used for
            predicting  field  life  and  operating  conditions.  Yale  et  al. 89  implemented  an
            improvement  to  their  reservoir  simulator  by  incorporating  a  variable  rock
            compressibility  into  a  reservoir  simulator,  but  that  modification  was  not  an
            implementation of full coupling.
              In some recent case studies, the solution of the governing equations has been
            simplified by assuming a steady-state solution for the pore pressure. The steady
            state  solution  is  still  coupled,  but  the  coupling  is  milder,  without  transient
            effects. Computing pore pressures with a standard uncoupled reservoir simulator
            been  used  as  a  further  simplification.  The  computed  pore  pressures  are
            prescribed  as  pore  pressure  boundary  conditions  at  discrete  intervals  of  time
            (e.g.,  yearly)  in  a  nonlinear  geomechanical  finite  element  model  and
            deformations are computed based on the effective stress. 37–40  In this approach, a
            sophisticated reservoir simulator was used to compute reservoir pressure based
            on the production and the injection of literally hundreds of wells, thus a highly
            heterogeneous  pore  pressure  field  was  used  in  the  finite  element  model  to
            compute compaction and its effects. However, this approach results in coupling
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