Phase fractionation and oil-condensate mass balance in the South Marsh Island Block 208–239 area, offshore Louisiana

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• 作者：Steven Losh ; Lawrence Cathles III
• 关键词：Gulf of Mexico ; Tiger Shoal ; Gas washing ; Evaporative fractionation ; Gas condensate ; Migration
• 刊名：Marine and Petroleum Geology
• 出版年：2010
• 出版时间：February 2010
• 年：2010
• 卷：27
• 期：2
• 页码：467-475
• 全文大小：1079 K

文摘

Phase fractionation can strongly deplete oil of its volatile compounds in a regular and characteristic fashion. This process has affected oils to a remarkably uniform extent throughout the 30 × 15 km South Marsh Island 208–239 and Vermilion 30–31 area (including the Tiger Shoal, Starfak, Mound Point, Lighthouse Point, Amber, Trinity Shoal, and Aquamarine fields) just offshore Louisiana. Fractionation of the original “parent” oil likely occurred in the deep, relatively flat-lying Rob L sand that underlies the area, and produced gas-washed oils (mean API 33°) and gas condensates (mean API 50°) in a volume ratio of 1:3.5. Both fractionated oil and vapor migrated from the fractionation site to shallower reservoirs. However, the estimated ultimate production ratio of gas-washed oil to gas condensate in this group of fields is 1:0.32, about 11 times higher than would be expected on mass balance considerations alone. Thus, there is an apparent deficiency of producible gas condensate relative to the amount of producible oil for the entire study area and for every field in that area. In the case of the Tiger Shoal field, the ratio of industry-estimated ultimately producible oil to gas condensate is 1:1.1. Based on the production data, we conclude that either there is an additional 6.4 × 10⁶ m³ (43 MMbbl) of undiscovered and/or unproduced condensate in the area or that condensate has escaped preferentially in vapor form to the seafloor. The well-studied and nearly depleted Tiger Shoal field provides a good example of how chemical data can be analyzed in a way that contributes insight into the phase fractionation process and the remaining exploration potential of an area.