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Record W958152525 · doi:10.11575/prism/27867

Stable Isotope and Geochemical Investigations into the Hydrogeology and Biogeochemistry of Oil Sands Reservoir Systems in Northeastern Alberta, Canada

2013· dissertation· en· W958152525 on OpenAlex
Benjamin R. Cowie

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.

aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenuePRISM (University of Calgary) · 2013
Typedissertation
Languageen
FieldEngineering
TopicHydrocarbon exploration and reservoir analysis
Canadian institutionsnot available
Fundersnot available
KeywordsBiogeochemistryHydrogeologyGeologyOil sandsGeochemistryStable isotope ratioEarth scienceHydrology (agriculture)OceanographyArchaeologyGeotechnical engineeringGeography

Abstract

fetched live from OpenAlex

The objective of this thesis was to provide insight into the hydrogeology and biogeochemistry of the heavily biodegraded bitumen reservoirs of the Athabasca oil sands region of Alberta, Canada, using applications of aqueous and stable isotope geochemistry. Published data were used to generate a regional map of total dissolved solids concentrations in McMurray Formation waters. To explain the regional salinity data, a revised hydrogeological model was developed that incorporates localized upward flow of formation waters from saline Devonian aquifers into the bitumen-bearing McMurray Formation via karst-derived conduits. Where McMurray Formation waters are uninfluenced by connectivity with Devonian aquifers, topographic recharge from meteoric water is the dominant hydrogeological process. A new method was developed to determine the stable isotope composition and salinity of McMurray Formation waters from porewater samples extracted from drilling fluid-contaminated core. Mixing relationships of δ2H and δ18O values in drilling fluid and formation water were used to calculate the original formation water stable isotope composition and salinity from porewater extracted directly from oil sands drill core. Both vertical and lateral heterogeneity were observed on a reservoir-scale, and topographically-derived groundwater recharge was determined to be the dominant hydrogeological process in Suncor-Firebag lease area. Biogeochemical aspects of oil sands systems were investigated in two studies. The first study examined the impact of variable aqueous geochemistry on oil sands biogeochemistry, specifically methanogenesis and bacterial sulfate reduction, in laboratory-scale microcosms. Changes in aqueous geochemistry induced changes in the total amount of methane generated, and in the stable isotope ratios of carbon and hydrogen of generated methane. The second experiment measured natural abundance radiocarbon in dissolved inorganic carbon in a coal-bed methane reservoir in the Powder River Basin, Montana, USA. All samples of dissolved inorganic carbon and methane contained no detectable radiocarbon, and thus the carbon flux from biodegradation of coal was much greater than the carbon flux from recent groundwater recharge into the coal-bed aquifer system. Improved understanding of hydrogeological processes, and better understanding of reservoir biogeochemistry will lead to better decision making by industry and regulators during the development of oil sands resources, while our society transitions away from fossil energy over the coming century.

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)0.000
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: Simulation or modeling · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.947
Threshold uncertainty score0.626

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 head0.005
GPT teacher head0.167
Teacher spread0.162 · 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