1. Banzala Development Plan: Overcoming the Shallow Gas Hazard
- Author
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M.E. Smith, M.K. Rieken, M.T. Gaona, D.J. Streu, and J. Sousa
- Subjects
Development plan ,Environmental science ,Hazard ,Environmental planning - Abstract
Abstract The Banzala Field, located offshore Cabinda, Angola, contains over one billion barrels of oil in place, in shallow water, at shallow depth and close to an existing infrastructure. The field was discovered in 1981, but the well was lost due to a blowout after reaching total depth. The blowout resulted in the charging of a very shallow interval with over-pressure gas that now completely overlies the deeper oil reservoirs. The gas pressure was unknown, but believed to be very close to fracture pressure. Exact areal extent of the gas was unknown and it was not known if the system was static or continuing to charge from a deeper gas sand. The field has not been developed because of the extent and uncertainty of shallow overpressured gas that overlies the deeper oil reservoirs and because of limited individual well productivity. It was surmised that the outer limit of the shallow gas or gas/water contact (GWC) should correspond to a structural contour elevation such that the corresponding hydrostatic head of sea water exactly balanced the pressure of the gas bubble. Hydrostatic pressure data dating from 1983 was used to boundgas pressure between a maximum and minimum value. Consequently, it was believed, the vertical subsea depth of the GWC was bounded. A dynamically positioned geotechnical vessel was chartered to drill along the calculated gas boundary. The effort was successful and appraisal wells have been drilled and evaluated. Low well productivity will be solved by closely spaced wells on electric submersible pump (ESP). Well downtime and pump pulling costs are being minimized by deploying theESPs on coil tubing. A "hard landing" area is being designed into the platforms to support coil tubing equipment spreads. Introduction The Banzala Field is located in Blocks 34, 35, 45, and 46 in Area A of the Cabinda Concession, offshore Angola, West Africa (Figure 1) in approximately 125 to 175 ft of water. The hydrocarbon accumulation at Banzala occurs in three primaryreservoirs (Mesa, Lago, and Azul) between -1600 ft and -2000 ft tvdss. It is estimated that these sands contain over one billion barrels of oil in place. The productive oil bearing reservoirs are overlain by the Frio and Landana gas sands. The Frio is a naturally occurring overpressured gas sand at -1000 ft tvdss. The Landana was originally normally pressured, but has been supercharged with gas as a result of the discovery well blowout in 1981. The Landana is between -425 and -600 ft tvdss. The Banzala Field is an anticline with four-way dip closure. The anticlinal structure (Figure 2) is well defined by six wells and 2seismic data. The crest of the anticlinal structure is difficult to resolve seismically because seismic data quality is locally degraded by shallow gas. Although amaximum of three faults have been mapped, additional faults that are not imaged with the current seismic data may be present.
- Published
- 1998
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