--> ABSTRACT: 4-D Seismic Monitoring of an Active Steamflood, by David E. Lumely, Michel Bee, Steve Jenkins, and Zhijing Wang; #91019 (1996)
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4-D Previous HitSeismicNext Hit Previous HitMonitoringNext Hit of an Active Steamflood

David E. Lumely, Michel Bee, Steve Jenkins, and Zhijing Wang

Multiple 3-D Previous HitseismicNext Hit surveys have been acquired at time-lapse intervals over a heavy oil Previous HitreservoirNext Hit in the Duri Field, Indonesia, to monitor the progress of an active steamflood. Time-lapse 3-D Previous HitseismicNext Hit images show dramatic and complex changes in the Previous HitreservoirNext Hit zone over a wide area, compared to baseline Previous HitseismicNext Hit data recorded prior to steam injection. Careful consideration of steamflood fluid-flow, rock physics measurements, finite-difference seismogram modeling, 3-D Previous HitseismicNext Hit imaging and velocity analysis leads to an integrated interpretation of this 4-D data set.

Anticipated large decreases in Previous HitseismicNext Hit P-wave velocity near the injection well correlate with the presence of a hot steam-saturated zone. Unanticipated large velocity increases and reflectivity changes in an annulus around the steam zone are consistent with a transient high-pressure front, in which initial free gas in pore space is raised above the bubble point pressure and dissolves into liquid oil. Horizontal and vertical anisotropy in flow directions inferred from these Previous HitseismicNext Hit observations correlate with two temperature monitor wells, and in situ measurements of upper and lower Previous HitreservoirNext Hit permeability. Since the pressure front propagates out from the injector at least one order of magnitude faster than either the thermal or steam fronts, Previous HitmonitoringTop it may be useful for predicting f owpaths of heated oil and steam, months in advance.

AAPG Search and Discover Article #91019©1996 AAPG Convention and Exhibition 19-22 May 1996, San Diego, California