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PSCurrent and Future Perspectives on Previous HitRecoveryNext Hit Growth from the Western Canada Sedimentary Basin*

By

Kirk G. Osadetz1 and Zhuoheng Chen1

 

Search and Discovery Article #10141 (2007)

Posted November 20, 2007

 

*Adapted from poster presentation at AAPG Annual Convention, Long Beach, California, April 1-4, 2007

 

1Geological Survey of Canada, 3303 33rd Street, NW, Calgary, Alberta, Canada, T2L 2A7 ([email protected])

 

Previous HitOilNext Hit Resource Base 

The Western Canada Sedimentary Basin (WCSB, senso lato including contiguous mainland Northwest Territories successions) hosts large proven and potential conventional and non-conventional Previous HitoilNext Hit resources. The ultimate recoverable reserve continues to grow. The basin is inferred to host an original in place conventional Previous HitoilNext Hit resource of ~26.6 x 109 m3 (168 x 109 bbls; Lee 1998; National Energy Board (NEB, 2001) (Figure 1), of which ~16.4 x 109m3 (103 x 109 bbls) has been discovered (CAPP, 2005). These resources have been variably altered, most significantly by biodegradation, and heavy Previous HitoilNext Hit is 7.9 x 109 m3 (50 x 109 bbls) of the original Previous HitoilNext Hit in place.

uPrevious HitOilNext Hit resource base

uFigure captions

uBitumen

uOther resources

uP & S Previous HitrecoveryNext Hit

uFuture Previous HitrecoveryNext Hit

uTertiary Previous HitrecoveryNext Hit

uWeyburn project

uReferences

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

uPrevious HitOilNext Hit resource base

uFigure captions

uBitumen

uOther resources

uP & S Previous HitrecoveryNext Hit

uFuture Previous HitrecoveryNext Hit

uTertiary Previous HitrecoveryNext Hit

uWeyburn project

uReferences

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

uPrevious HitOilNext Hit resource base

uFigure captions

uBitumen

uOther resources

uP & S Previous HitrecoveryNext Hit

uFuture Previous HitrecoveryNext Hit

uTertiary Previous HitrecoveryNext Hit

uWeyburn project

uReferences

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

uPrevious HitOilNext Hit resource base

uFigure captions

uBitumen

uOther resources

uP & S Previous HitrecoveryNext Hit

uFuture Previous HitrecoveryNext Hit

uTertiary Previous HitrecoveryNext Hit

uWeyburn project

uReferences

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

uPrevious HitOilNext Hit resource base

uFigure captions

uBitumen

uOther resources

uP & S Previous HitrecoveryNext Hit

uFuture Previous HitrecoveryNext Hit

uTertiary Previous HitrecoveryNext Hit

uWeyburn project

uReferences

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

uPrevious HitOilNext Hit resource base

uFigure captions

uBitumen

uOther resources

uP & S Previous HitrecoveryNext Hit

uFuture Previous HitrecoveryNext Hit

uTertiary Previous HitrecoveryNext Hit

uWeyburn project

uReferences

 

 

 

 

 

 

Figure Captions

Figure 1. Geographic distribution of Canadian crude Previous HitoilNext Hit (area of circle proportional to initial in-place resource), bitumen and tar sands resources (area of circle proportional to current official reserve estimate). The majority of the resource occurs in the Western Canada Sedimentary Basin, south of 60o N. This presentation addresses Previous HitenhancedNext Hit Previous HitrecoveryNext Hit potential only in that region.

Figure 2. Photo of Weyburn field facilities.

Figure 3. Illustration of successive CO2 and water slugs injected at Weyburn.

Figure 4. Map of the Western Canada Sedimentary Basin, indicating the thickness of the succession and the location of select planned, current, and historical programs of Tertiary Previous HitrecoveryNext Hit (generalized).

Figure 5. Production history and projections for the Weyburn field, distinguishing incremental improvements associated with various project phases. 

 

Previous HitOilNext Hit Resource Base (Bitumen) 

Alberta original in place bitumen accumulations are confidently estimated to be ~269 x 109 m3 (1.7 x 1012 bbls; Marsh, 2006; AEUB, 2006; Procter et al., 1984, p. 48). Alberta original in-place bitumen reserves are estimated ~28.4 x 109 m3, (179 x 109 bbls; Marsh, 2006; AEUB, 2006), although this may increase. The official estimate of bitumen reserves includes industrially recognized reserves that comprise at least 2.6 x 109 m3 (16 x 109 bbls; CAPP, 2005) initial in-place in-situ bitumen, with no primary Previous HitrecoveryNext Hit, and surface mineable bitumen accumulations of ~1.44 x 109m3 (9 x 109 bbls; CAPP, 2005).

 

Previous HitOilNext Hit Resource Base (Other Resources) 

Tertiary Previous HitrecoveryNext Hit of conventional oils is a minor effort, in part because of history, availability, and the cost of miscible fluids, but new efforts (Figures 2 and 3) are providing a previously ignored potential conventional Previous HitoilNext Hit resource, which competes for attention with the non-conventional resources.  

Tertiary Previous HitrecoveryNext Hit efforts also compete with other potential non-conventional resources. Currently there are neither significant shale-Previous HitoilNext Hit nor Previous HitoilNext Hit-shale developments, although potential exists for both. Major bituminous shales occur across the WCSB, with the most significant occurring in Devonian Duverney, Devonian and Carboniferous Bakken/Exshaw, Jurassic Fernie, Upper Cretaceous Boyne and Favel (white speckled shales equivalent to Greenhorn and Niobrara) formations (Creaney et al., 1994). These formations produce small conventional volumes, but the shale-Previous HitoilNext Hit resource is neither well described nor exploited. Some bituminous formations are mineable Previous HitoilNext Hit shales, the upper Cretaceous being most important. There is no Previous HitoilNext Hit-shale resource estimate; yet outcrops are commonly 20-40 m thick, extending over hundreds of kilometres. Yields up to 100 litres Previous HitoilNext Hit/tonne were obtained from the Pasquia Hills, Manitoba (Macauley, 1984). Immense coal resources (Smith, 1989) host natural gas from coal that has begun to augment the gas supply. A reliable natural gas supply is important for several Previous HitrecoveryNext Hit technologies, particularly for bitumen, but in the future these coals may also be a source for synthetic Previous HitoilNext Hit.

 

Current Primary and Secondary Previous HitRecoveryNext Hit: 

Most production employs primary natural depletion, or secondary Previous HitrecoveryNext Hit, most commonly pressure maintenance. Primary Previous HitrecoveryNext Hit factors vary. The average WCSB primary RF is ~14%. The average is lower for heavy oils, where primary Previous HitrecoveryNext Hit can be 5% or lower. Typically, primary recoveries are ~16% for Paleozoic carbonates and even higher, exceeding 19%, for non-biodegraded Mesozoic reservoirs. Secondary Previous HitrecoveryNext Hit commonly adds an incremental 4%-10% Previous HitrecoveryNext Hit. Secondary Previous HitrecoveryNext Hit can be spectacularly effective, as in the Northwest Territories, where production comes primarily from Devonian carbonates and most of that from the Norman Wells reef. There secondary Previous HitrecoveryNext Hit increased the Previous HitrecoveryNext Hit from the 16% typical of Paleozoic carbonates to 46%, adding an incremental 15.2 x 106m3 (96 x 106 bbls). Elsewhere secondary Previous HitrecoveryNext Hit results are more modest. Most of the incremental 957.8 x 106m3 (6,034 x 106 bbls) from secondary Previous HitrecoveryNext Hit is from Alberta, where secondary Previous HitrecoveryNext Hit identified an incremental 652.0 x 106m3 (4,108 x 106 bbls). In Saskatchewan 4% or 233.9 x 106m3 (1,473 x 106 bbls) has been added mostly from Carboniferous subcrop pools. The use of secondary schemes in Manitoba has been negligible and only 1% or 1.3 x 106m3 (8 x 106 bbls) is attributable to secondary Previous HitrecoveryNext Hit.

 

Future Previous HitRecoveryNext Hit: 

The WCSB is a potential target for established and new Previous HitrecoveryNext Hit and stimulation technologies, including, miscible floods, simulated horizontal wells, and SAGD/JIVE. A recent Previous HitoilNext Hit supply model (NEB, 2006) suggests WCSB Previous HitoilNext Hit supply will increase from 2005 volumes of 365 x 103m3/day (2.3 x 106 bbls/day) to 613 x 103m3/day (3.9 x 106 bbls/day) by 2015, due to increased bitumen production alone. The model suggests that conventional Previous HitoilNext Hit production will decline in spite of improved Previous HitrecoveryNext Hit (NEB, 1999; 2003). Still, the model suggests that future improvements in conventional light and heavy Previous HitrecoveryNext Hit will contribute 722 x 106m3 to 794 x 106m3 (4.55 x 109 bbls to 5.00 x 109 bbls; NEB 1999; 2003; CAPP, 2005). This represents an incremental 16%-19% increase in Previous HitrecoveryNext Hit and a volume comparable to the remaining established reserve. It implies that average Previous HitrecoveryNext Hit factor increases from 21%, currently, to 27.5%. The NEB (2001) increased conventional heavy Previous HitoilNext Hit 30% over previous resource estimates (Lee, 1998), and both heavy-Previous HitoilNext Hit and Previous HitoilNext Hit-sand resource bases may increase as technology develops. Shale Previous HitoilNext Hit and Previous HitoilNext Hit shale are not yet part of supply, and their input could add significantly to Previous HitrecoveryNext Hit growth. While encouraging, it will require much study and many more projects to know if the inferred Previous HitrecoveryNext Hit improvements can be commercial.

 

Current Tertiary Previous HitRecoveryNext Hit: 

Aside from a few projects, often technology demonstrations, tertiary Previous HitrecoveryNext Hit has not been applied widely (Figure 4). Overall, to the end of 2004, tertiary Previous HitrecoveryNext Hit produced only an incremental 209.0 x 106m3 (1,317 x 106 bbls) accounting for less than one percent increase in Previous HitrecoveryNext Hit. Some regions, notably Manitoba, British Columbia, and the Northwest Territories have effectively no contribution from tertiary programs. This is not indicative of the tertiary programs, but rather it indicates the lack of their application. Tertiary programs have been historically restricted to Alberta, where projects added an incremental 176.9 x 106m3 (1,071 x 106 bbls), resulting in a 2% increase in reserves. Alberta tertiary Previous HitrecoveryNext Hit projects do not include in-situ Previous HitoilNext Hit sands projects, such as cyclic steam stimulation project at Cold Lake, or Steam Assisted Gravity Drainage (SAGD) projects, which produced 203.5 x 106m3 (1,282 x 106 bbls) bitumen by the end of 2004 (CAPP, 2005), all of which is attributed to tertiary Previous HitrecoveryNext Hit. The recoverable reserve of in-situ Previous HitoilNext Hit sands 534.8 x 106m3 (3,369 x 106 bbls), is a small fraction of the initial in-place bitumen (ibid.).

 

Weyburn and Midale Projects 

In Saskatchewan, the small incremental volume, 32.0 x 106m3 (202 x 106 bbls) from tertiary programs conceals the importance of the Weyburn CO2 sequestration and tertiary  Previous HitrecoveryNext Hit project (Figures 2, 3, 5). The project, in a Carboniferous carbonate pool, will produce an incremental 20.6 x 106m3 (130 x 106 bbls), using miscible or near-miscible CO2 displacement  from a pool that produced 53.2 x 106m3 Previous HitoilNext Hit (335 x 106 bbls) since 1955. Important Previous HitrecoveryNext Hit improvements accompanied the in-fill drilling program that preceded the CO2 flood. The  project extends field life by ~25 years, and Previous HitrecoveryNext Hit factor improves ~28%, from the CO2 flood alone. It will permanently sequester ~20 million tonnes CO2. Plans are underway to apply a similar scheme of Previous HitenhancedNext Hit Previous HitrecoveryNext Hit to the nearby and geologically similar Midale Field.

 

References 

AEUB, 2006, Alberta's reserves 2005 and supply/demand outlook 2005/2015: Alberta Energy and Utilities Board, Calgary, CD-ROM.

CAPP (Rodriguez, S. content coordinator), 2005, Statistical Handbook 2005: Canadian Association of Petroleum Producers, Calgary, CD-ROM.

Creaney, S., Allan, J., Cole, K.S., Fowler, M.G., Brooks, P.W., Osadetz, K.G., Macqueen R.W., Snowdon, L.R., Riediger, C.L., 1994, Petroleum generation and migration in the western Canada Sedimentary Basin (Chapter 32), in G. Mossop and I. Shetsen (compilers), Geological Atlas of the Western Canada Sedimentary Basin: Canadian Society of Petroleum Geologists and Alberta Research Council, Calgary and Edmonton, p 455-470.

Lee, P.J., 1998, Previous HitOilNext Hit resources of Western Canada: Geological Survey of Canada, Open File Report, 3674, 142 p.

Macauley, G., 1984, Geology of the Previous HitoilNext Hit shale deposits of Canada: Geological Survey of Canada Paper 81-25, 65 p.

NEB, 1999, Canadian energy supply and demand 1999 to 2025: National Energy Board of Canada, Calgary, 96 p.

NEB, 2001, Conventional heavy Previous HitoilNext Hit resources of the Western Canada Sedimentary Basin: Technical Report, National Energy Board of Canada, Calgary, 96 p.

NEB, 2003, Canadian energy supply and demand 2003 to 2025 (update of the 1999 report of the same name dealing primarily with errata): National Energy Board of Canada, Calgary, 96 p.

NEB, 2006, Canada's Previous HitoilNext Hit sands: Opportunities and challenges to 2015: An update. Energy Market Assessment June 2006, National Energy Board of Canada, Calgary, 71 p.

Procter, R.M., Taylor, G.C., and Wade, J.A., 1984, Previous HitOilNext Hit and natural gas resources of Canada 1983: Geological Survey of Canada, Paper 83-31, 59 p.

Smith, G.G., 1984, Coal resources of Canada: Geological Survey of Canada Paper 89-4, 146 p.

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