| AOGCC Pool Statistics |
Prudhoe Bay Unit, Prudhoe Oil Pool |
| Operator: | BP Exploration (Alaska) Inc. | ![]() | |
| Discovery Well: | Arco Alaska Inc. | ||
| Prudhoe Bay State No. 1 | |||
| Permit No. 167-011 | |||
| API No. 50-029-20001-00-00 | |||
| Sec.10, T11N, R14E, UM | |||
| Depth: 12,005’ MD / 12,005' TVD | |||
| December 19, 1967 |
| Status: | Producing | ||||
| Location: | Central Arctic Slope | Area Location Map | Pool Location Map | DNR Unit Map | |
| Orders: | List of Orders | Summary - Annotated | References | ||
| Summary: | Prudhoe Bay is the largest oil field in North America, and it ranks among the 20 largest fields in the world. The operator, BP, estimates the original oil in place to be about 25 billion barrels, and gas in place is estimated to be 46 trillion cubic feet. As of February 2011, field production totaled nearly 11.3 billion barrels of oil. Associated produced water and most of the associated produced gas are currently re-injected to maintain reservoir pressure. The Prudhoe Bay State No. 1 exploratory well discovered this pool in 1968. In that well, DST No. 12 (a 48-1/2 hour production test that began June 1, 1968) produced oil at a maximum rate of 2,415 barrels per day, with an average estimated rate of about 2,025 barrels per day. | ||||
| Geology: | The Prudhoe Oil Pool is defined as the accumulations of oil that are common to and which correlate with the accumulations found in the Atlantic Richfield - Humble Prudhoe Bay State No. 1 well between the depths of 8,110 and 8,680 feet. The Prudhoe Bay, Prudhoe Oil Pool encompasses, in ascending order, the Sadlerochit, Shublik and Sag River Formations. The Sadlerochit Formation is Triassic-aged, and it consists of 300 to 600 feet of sandstone and conglomerate. The lower part of the Sadlerochit consists of a basal, prodelta marine unit that grades upward into a marginal marine coastal sequence consisting of interbedded sandstone and shale. The upper part was deposited by rivers and braided streams in a nonmarine alluvial environment. Most of the recoverable reserves of the Sadlerochit occur in these braided stream sediments, where porosity ranges from 20 to 24% and permeability ranges from 300 md to several darcys. The Shublik Formation is also Triassic-aged, and it consists of organic- and phosphate-rich sandstone, muddy sandstone, mudstone, silty limestone, and limestone. These sediments were deposited in a low energy marine environment with high biologic productivity. The Sag River Formation consists of a lower sandstone member and an upper shale member. The sandstone member consists of uniform, well-sorted, fine-grained sandstone and siltstone that were deposited within a barrier beach complex. The Sag River Formation forms a relatively continuous reservoir over a large part of the Prudhoe Bay Field. The sandstone member thickens from 20’ in the south to about 70’ in the north, and reservoir conditions improve toward the northeast. Porosity and permeability average about 25% and 270 md, respectively. The overlying shale member consists of shale and mudstone. This member thins from about 70’ in the west to about 10’ in the main field area. | ||||
| Strat Column | Type Log | ||||
| Production: | Prod Chart |
| Oil (bbls) | NGL (bbls) | Gas (mcf) | Water (bbls) | |
| Cumulative | 11,279,570,171 |
560,884,213 | 63,944,034,268 | 9,340,375,795 |
2005 Total |
118,480,580 | 21,419,504 | 2,823,410,898 | 412,604,527 |
2006 Total |
91,356,646 | 19,266,361 | 2,444,754,420 | 286,125,040 |
2007 Total |
95,480,242 | 20,704,755 | 2,703,931,559 | 330,826,590 |
2008 Total |
95,839,407 | 19,201,129 | 2,653,723,548 | 350,017,225 |
2009 Total |
91,244,587 | 18,423,385 | 2,613,671,942 | 325,757,858 |
2010 Total |
88,823,023 | 16,675,601 | 2,517,686,819 | 320,550,842 |
2011 Total |
0 | 0 | 0 | 0 |
2007 Rate (b/d) |
261,590 | 56,725 | 7,408,032 | 906,374 |
2008 Rate (b/d) |
262,574 | 52,606 | 7,270,475 | 958,951 |
2009 Rate (b/d) |
249,985 | 50,475 | 7,160,745 | 892,487 |
2010 Rate (b/d) |
243,351 | 45,687 | 6,897,772 | 878,221 |
| 2011 Rate (b/d) | 0 | 0 | 0 | 0 |
2008 Change (%) |
0 | -7 | -2 | 6 |
2009 Change (%) |
-5 | -4 | -2 | -7 |
2010 Change (%) |
-3 | -9 | -4 | -2 |
2011 Change (%) |
0 | 0 | 0 | 0 |
