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production  of  a  reservoir  and  also  by  natural  conditions.  A
          particular  mechanism  of  a  reservoir  drive  may  be  established,
          maintained,  controlled  and  even  replaced  by  a  different
          mechanism. It depends to a large extent on the rate of fluid and gas
          withdrawals  and  on  artificial  measures  carried  out  during  the
          exploitation of the reservoir (such as injecting a driving agent into
          the  reservoir).  Geological  conditions  and  the  specific  source  of
          formation  energy  only  help  to  establish  a  particular  driving
          mechanism but do not only fully determine it.
                  Elastic  drive.  Condition  elastic  drive  -  excess  reservoir
          pressure above the saturation pressure. Bottom-hole pressure is not
          less than the saturation pressure.
                  Oil is a single-phase state. The influx of oil to the wells is
          due to the elastic properties of reservoir rocks and fluids.
                  In the case of an elastic-water drive, the changes observed
          in  the  reservoir  behaviour  are  of  a  different  nature.  A  typical
          feature  of  the  elastic-water  drive  mechanism  is  a  decline  in
          pressure during the initial period. Thereafter, if fluid withdrawals
          remain constant, the rate of pressure decline tapers off. This is due
          to the fact that with time, the zone of reduced pressure extends to
          an ever-increasing area of the reservoir, and to  maintain a given
          influx of fluid by the elastic expansion of the reservoir rocks and
          fluids  a  smaller  pressure  decline  is  required  than  in  the  initial
          period. If the bottom-hole pressure is maintained constant, the flow
          at  the  wells  at  first  diminishes  rapidly,  but  later  on,  the  rate  of
          decrease tapers off. The elastic properties of reservoir rocks and
          fluids  are  nicely  characterised  by  the  fact  that  any  change  in
          pressure at any point in the reservoir is not transmitted through the
          formation instantaneously but at a certain rate (Fig. 2.2).











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