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Record W1999821497 · doi:10.2118/163079-pa

Understanding the Heat-Transfer Mechanism in the Steam-Assisted Gravity-Drainage (SAGD) Process and Comparing the Conduction and Convection Flux in Bitumen Reservoirs

2013· article· en· W1999821497 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.
aboutThe title or abstract carries a Canadian signal from the geographic lexicon.

Bibliographic record

VenueSPE Journal · 2013
Typearticle
Languageen
FieldEngineering
TopicEnhanced Oil Recovery Techniques
Canadian institutionsUniversity of Alberta
Fundersnot available
KeywordsThermal conductionHeat transferConvectionConvective heat transferHeat fluxMechanicsSteam injectionNatural convectionGeologyForced convectionSteam-assisted gravity drainageThermalAsphaltPetroleum engineeringThermodynamicsOil sandsMaterials sciencePhysics

Abstract

fetched live from OpenAlex

Summary SAGD is one successful thermal recovery technique applied in the Athabasca and Peace River reservoirs in central and northern Alberta, Canada. In SAGD, steam is injected into a horizontal injection well and is forced outward, losing its latent heat when it comes into contact with the cold bitumen at the edge of a depletion chamber. As a consequence, the viscosity of the bitumen falls several orders of magnitude, its mobility rises several orders of magnitude, and then it flows under gravity toward a horizontal production well located several meters below and parallel to the injection well. Heat-transfer mechanisms are pivotal to the SAGD process. Though heat energy is transferred from steam to reservoir by conduction and convection, heat transfer by convection is not considered in the classic SAGD mathematical models such as Butler?s. Researchers such as Butler and Stephens (1981), Reis (1992), Akin (2005), Liang (2005), Nukhaev et al. (2006), and Azad and Chalaturnyk (2010) considered conduction from steam to cold reservoir to be the only heat-transfer component. However, because the heat capacity of water is typically two to five times that of bitumen, convection caused by the mobile condensate flow in the reservoir may contradict these studies. Farouq-Ali (1997) was the first to criticize the assumption that there is only a thermal conduction mechanism in the SAGD process. He pointed out that with so much condensate flowing, convection would be expected to be the dominant heat-transfer mechanism, which can be plausible at high temperatures. In response, Edmunds (1999a) stated that on the basis of the associated change in enthalpy, the heat transfer into a cold reservoir because of convection is probably less than 5% of that because of conduction. Ito (1999) challenged Edmunds (1999a) statement, on the basis of Ito and Suzuki (1996, 1999) and Ito et al. (1998), pointing out that "this number, 5%; i.e., ratio between convection to conduction presented by Edmunds (1999a) is unrealistically low, (and) it should be in the range of 50%. This study examined the relative roles of convective and conductive heat transfer at the edge of SAGD steam chambers. In summary, the mathematical model developed in this study considered both conduction and convection, and the resultant output from the model is reasonably consistent with published field data. This study supports the idea that although convection can dominate near the chamber edge in high-water-saturation reservoirs, in bitumen-rich reservoirs, its contribution to heat transfer is less than 1% and can be neglected.

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.

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)0.001
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Theoretical or conceptual · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.602
Threshold uncertainty score0.320

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0010.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.001
Insufficient payload (model declined to judge)0.0000.000

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 head0.046
GPT teacher head0.255
Teacher spread0.209 · 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