Page 179 - Principles of Applied Reservoir Simulation 2E
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164  Principles of Applied  Reservoir Simulation


        small blocks. An LGR grid is an example of a flexible or unstructured grid. A
        flexible grid is made up of polygons in 2D (polyhedra in 3D) whose shape and
        size vary from  one subregion to another in the modeled region.
             Although many grid preparation  options  are available,  improving grid
        preparation  capability  is  an  on-going  research  and  development  topic.  For
        example, not all flow simulators use a finite difference  formulation. Some are
        based on a control volume finite element formulation that use triangular meshes
        in 2D (tetrahedral meshes in 3D). Finite difference grids typically display global
        orthogonality in which the grid axes are aligned  along orthogonal coordinate
        directions.  Examples  of globally orthogonal coordinate  systems  include the
        Cartesian x-y-z  system  and  the  cylindrical r-Q-z  system.  Grids  with global
        orthogonality  may be distorted  to  fit  local  irregularities  such  as  faults  using
        corner-point geometry. By contrast, finite element grids display orthogonality
        in which gridblock boundaries are perpendicular to lines joining gridblock nodes
        on opposite  sides of each boundary. An example of a locally orthogonal grid
        is a perpendicular bisector (PEBI) grid. Aziz [ 1993], Chin [1993], Heinemann
        [ 1994], Verma and Aziz [ 1997], and Heinemann and Heinemann [ 1998] provide
        additional discussion of grid preparation research.



                                 16.3  Model Types

             Models  may be  classified  into three different  types:  full  field  models,
        window area models, and conceptual models. Full field models are used to match
        performance of the entire field. They take into account the interaction between
        all wells and layers. The results of full field models are already matched to field
        scale and require no further scaling. The disadvantage of using full field models
        is that the number of grid blocks may need to be large or the grid size may need
        to be relatively coarse to include the entire field.
             Window area models are designed to look at smaller areas of the field.
        These models are often  constructed from a full field description.  Window area
        models allow finer grid resolution or shorter turnaround time if the model runs
        faster than a full field model. The window area models are useful  for studying
        recovery mechanisms and for determining reasonable grid preparation  criteria
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