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Record W2309158614 · doi:10.2118/174464-ms

Production of Gases During Thermal Displacement Tests

2015· article· en· W2309158614 on OpenAlexafffund
Jessica Butron, J. Bryan, Xiaoli Yu, Apostolos Kantzas

Bibliographic record

VenueSPE Canada Heavy Oil Technical Conference · 2015
Typearticle
Languageen
FieldEngineering
TopicEnhanced Oil Recovery Techniques
Canadian institutionsUniversity of Calgary
FundersNatural Sciences and Engineering Research Council of CanadaAlberta InnovatesCMG Reservoir Simulation Foundation
KeywordsCarbonatePetroleum engineeringAsphaltThermalVolume (thermodynamics)Carbon dioxideFossil fuelDisplacement (psychology)Core (optical fiber)MineralogyEnvironmental scienceGeologyGeotechnical engineeringMaterials scienceWaste managementChemistryComposite materialThermodynamicsEngineeringMetallurgy

Abstract

fetched live from OpenAlex

Abstract During laboratory testing of thermal processes (hot water and steam displacement of bitumen) a consistent observation has been the production of very high gas volumes with produced oil and water. These gases are many times more in volume than what is expected from solution GOR and what is observed in the field. This paper presents an ensemble of experimental results of thermal displacement tests in oil sand and bitumen bearing carbonate rocks. The focus of analysis of these tests deals with the generation of non-condensable gases. Various laboratory core floods are run over a temperature range of 160 – 200°C+. Tests are run on native-state oil sand and carbonate samples, containing original saturations of bitumen and connate water. Cores are exposed to either hot water or steam, in linear flooding configurations or soaking conditions. The output from these tests is a measurement of produced gas volumes and compositions as a function of either soaking time or volumes of water/steam injected through the core. Tests were conducted on McMurray oil sand, Grand Rapids oil sand, and carbonate systems. During thermal displacements and at temperatures as low as 160°C, gases are generated. The gases are predominantly CO2 and H2 with traces of CH4 (which is usually seen early in the experiments) and other low carbon hydrocarbons. The last ones are usually at the noise level of the analytical instruments. What is significant is that at the lower temperatures there is no apparent generation of H2S and that supports the fact that the gas generation process is not aquathermolysis driven. The generation of gases is apparent in bitumen rich and bitumen free samples. This supports the assumption that the generation of gases is geochemical in nature, as well as through organic decomposition. The conclusion of the analysis indicates that the generation of such gases is caused by the combined effects of water/oil and water/solids reactions. Gas generation is affected by the system conditions and in general higher gas volumes are produced at lower P/Psat. Gas production is also strongly affected by surface contact between water and solids, which leads to lower apparent gas generation rates in carbonates compared to oil sands, and higher gas production from floods compared to soaking tests. The effect of such reactions in the exploitation of clay bearing sands and carbonate rocks is that the generation of extra gases will affect the thermodynamics (partial pressures), heat transfer (insulation) and relative permeability curves of the intended processes (SAGD, CSS, SAGD-solvent).

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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Bench or experimental · Consensus signal: Bench or experimental
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.213
Threshold uncertainty score0.983

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
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 integrity0.0000.000
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 head0.020
GPT teacher head0.237
Teacher spread0.217 · 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.

The models applied no category: nothing in the taxonomy fit this work.
Study designBench or experimental
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

Citations9
Published2015
Admission routes2
Has abstractyes

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