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Record W1969519716 · doi:10.1190/urtec2013-085

Integrated Geological Reservoir Characterization of the Cardium Light Tight Oil Play, Pembina Field in Alberta

2013· article· en· W1969519716 on OpenAlexaffabout
Per Kent Pedersen, Adam Fraser

Bibliographic record

VenueUnconventional Resources Technology Conference, Denver, Colorado, 12-14 August 2013 · 2013
Typearticle
Languageen
FieldEngineering
TopicHydrocarbon exploration and reservoir analysis
Canadian institutionsUniversity of Calgary
Fundersnot available
KeywordsCharacterization (materials science)Tight oilReservoir modelingGeologyPetroleum engineeringField (mathematics)Oil fieldPetrologyMaterials scienceNanotechnologyPaleontology

Abstract

fetched live from OpenAlex

Summary URTeC 1619723 Marine muddy sandstones of the Cardium Formation is the most active light tight oil play in western Canada, with production from the new multistage horizontal wells exceeding 120,000 bbl/d. Cardium sandstones contain one of largest oil accumulations in the Western Canada Sedimentary Basin, which have been exploited since the mid 1950’s. Since 2008 the play has been revitalized with activity mainly focused around the halo area of legacy pools, targeting low porosity and permeability muddy, intensely bioturbated sandstone reservoirs. This study presents a pore to depositional sequence scale reservoir characterization of the unconventional type low permeability, intensely bioturbated offshore to transitional offshore reservoir facies. The characteristics of the eastern and western Pembina halo play areas are presented and contrasted. Although they contain similar sedimentary facies they have very different reservoir properties due to differences in burial depth and thereby diagenesis, compaction, cementation, pore characteristics and reservoir pressure. Facies belt and thereby reservoir fairway widths of offshore deposits are often portrayed as being 10s of km wide, however mapping within a 5th order high resolution sequence stratigraphic framework shows that the offshore facies belts within the Pembina area are commonly less than a few km wide. Thus, a horizontal well drilled perpendicular to shoreline orientation might be landed in different reservoir facies. The 5th order sequences form in west Pembina part of a 3th order falling stage systems tract, characterized by basinward shift of facies. In contrast, the sequences in the eastern Pembina halo area form part of a late lowstand to early transgressive 3 order systems tract. Reservoir properties of intensely bioturbated reservoirs are poorly characterized by routine core analysis due to their highly heterogeneous character. In this study, detailed core observations were complemented with thin section, SEM analysis, mercury (MICP) data of the various micro facies, i.e. muddy matrix versus sandy borrow fill. Full core diameter CT scanning were used to characterize the 3-D connectivity of the sandstone beds and sandstone filled borrows for each reservoir facies. Due to the small scale and discontinuous of the sandstones, routine plug and full diameter core analysis often underestimate the flow capacity of such intensely bioturbated reservoirs, where sand filled borrow provides flow pathways in 3-D.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow), Insufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.387
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0010.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0010.001
Insufficient payload (model declined to judge)0.0030.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.008
GPT teacher head0.192
Teacher spread0.184 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one teacher head, not a consensus.

Study designNot applicable
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations2
Published2013
Admission routes2
Has abstractyes

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