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PERFORMANCE OF CONVENTIONAL OIL AND GAS RESERVOIRS              277
            14.3.1  Wilmington Field, California: Immiscible Displacement by
            Water Flooding
            A water flood uses injection wells to inject water into a reservoir. The injected water
            provides pressure support and can displace oil. A pattern water flood uses injection and
            production wells in a repeating pattern. The performance of the Wilmington Field in
            California (see Figure 14.3) illustrates immiscible displacement by water flooding.
              The Wilmington Field is in the Los Angeles Basin and was discovered in 1932 as
            part of the development of the Torrance field. The Wilmington Field was first recog‑
            nized as a separate field in 1936. The field is a northwest to southeast trending
              anticline that is approximately 13 mi. long and 3 mi. wide. It is crosscut into fault
            blocks that are vertically separated by normal faults that are perpendicular to the
            long axis of the anticline. The southeastern part of the field is beneath Long Beach
            Harbor and is called the Long Beach Unit (LBU). Otott and Clark (1996) reported
            that the Wilmington Field contained approximately 8.8 billion barrels of original
            oil in place (OOIP). The OOIP of the LBU of the Wilmington Field is greater than
            3 billion barrels.
              Seven stratigraphic zones have been identified between 2000 and 7500 ft true
            vertical depth subsea (TVDSS). From shallowest to deepest, the zones are the Tar,
            Ranger, Upper Terminal, Lower Terminal, Union Pacific, Ford, and “237.” An uncon‑
            formity lies above the Tar zone and another unconformity lies below the “237” zone.
            The zones and some fault blocks are sketched in Figure 14.4 (Fanchi et al., 1983;
            Clarke and Phillips, 2003).
              The upper six zones consist of unconsolidated to poorly consolidated sandstones
            interbedded with shales and exhibit high compaction characteristics. Surface
              subsidence up to 29 ft was observed as a result of producing the onshore part of the








                                             North           California

                 Pacific       Torrance
                 Ocean


                                                                Los Angeles
                                                                   Basin


                         Wilmington Field
                                                Belmont
                                                Offshore



                            FIgURE 14.3  Wilmington Field, California.
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