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TitleA re-evaluation of Beaufort Sea-Mackenzie Delta basin gas hydrate resource potential: petroleum system approaches to non-conventional gas resource appraisal and geologically-sourced methane flux
AuthorOsadetz, K G; Chen, Z
SourceBulletin of Canadian Petroleum Geology vol. 58, 1, 2010 p. 56-71, https://doi.org/10.2113/gscpgbull.58.1.56
Year2010
Alt SeriesEarth Sciences Sector, Contribution Series 20100276
PublisherGeoScienceWorld
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf
ProvinceNorthwest Territories; Northern offshore region
NTS107C
AreaBeaufort Sea; Mackenzie Delta
Lat/Long WENS-136.0000 -132.0000 70.0000 69.0000
Subjectsfossil fuels; hydrocarbon gases; hydrocarbons; hydrocarbon potential; hydrate; methane; exploration history; petroleum resources; resources; resource estimation
Illustrationslocation maps; tables; graphs; plots
Released2010 07 14
AbstractArctic gas hydrates (GH) sequester large volumes of natural gases. New Beaufort Sea-Mackenzie Delta Basin (BMB) permafrost and geothermal gradient maps motivate the revision of the gas hydrate stability zone (GHSZ) and re-evaluation of BMB GH resources using two independent, petroleum system-based resource models. The first model is both deterministic and spatial, and it is based on the quantitative analysis of both GH occurrences and reservoir characteristics. In addition, a spatial density of structural elements parameter that is well correlated to GH occurrences is used as a proxy for petroleum migration into the GH stability zone for the purpose of guiding the interpolation of GH occurrences between wells. The second GH resource model is probabilistic. Like the deterministic resource model, it permits regional resource characterization as a function of reservoir parameters that are potential proxies for technological and economic supply requirements. The total resource potential mapped deterministically is 8.82 × 1012 m3 raw initial natural gas in place (GIP). Geographic resource variations are illustrated by GHs maps exceeding specified characteristics as illustrated by GH saturation (Sgh), which is a potential proxy for reservoir energy. If the average Sgh is either >30% or >50%, then the inferred GH resource volumes are 6.40 × 1012 m3 and 4.59 × 1012 m3 GIP, respectively. The probabilistic GH resource appraisal predicts an expected total resource = 10.23 × 1012 m3 GIP. Similarly, if the average Sgh is either >30% or >50%, then the respective GH resource volumes inferred probabilistically are expected to be 6.93 × 1012 m3 and 4.20 × 1012 m3 GIP, respectively, which is comparable to the deterministically mapped estimates. Methane sequestered in GHs constrains regional, long-term, geologically-sourced methane flux rates. The BMB long-term regional methane flux sequestered in GHs is certainly <4.20 mg/m2/d and more likely not >0.12 mg/m2/d, whereas a single active thermogenic natural gas seep has a discharge of approximately 3.9 × 103 mg/m2/d. Although additional study is required before the atmospheric contribution from BMB geologically-sourced methane can be assessed, it is clear that:
1) much more thermogenic methane migrates into the GHSZ, or higher, than is trapped in the conventional resource;
2) the current atmospheric natural gas flux at point seeps can exceed greatly the long-term regional flux sequestered in the GHSZ, and;
3) the GHSZ is an imperfect trap.
GEOSCAN ID287170