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Record W2158985230 · doi:10.1016/j.egypro.2009.02.075

Geological model and hydrogeological framework of an active CO2 sequestration project in the Weyburn–Midale area, Saskatchewan: Leading to a further understanding of possible CO2 migration

2009· article· en· W2158985230 on OpenAlexaffabout
Gavin Jensen, Erik H. Nickel, Steve Whittaker, Ben Rostron

Bibliographic record

VenueEnergy Procedia · 2009
Typearticle
Languageen
FieldEnvironmental Science
TopicCO2 Sequestration and Geologic Interactions
Canadian institutionsUniversity of AlbertaPetroleum Technology Research CentreGovernment of Saskatchewan
Fundersnot available
KeywordsHydrogeologyAquiferAnhydriteGeologyCaprockGeomechanicsEvaporitePetroleum engineeringGeochemistryPetrologyGroundwaterGeotechnical engineeringGypsumSedimentary rock

Abstract

fetched live from OpenAlex

The current phase of the IEA Weyburn–Midale CO2 Monitoring and Storage Project is focused on building upon the rich dataset and experience developed during Phase I to provide additional understanding of parameters important to developing and implementing greenhouse gas storage sites. During the final phase, a revised, static geocelluar model will serve as the heart of the data storage component of the project that can be used by researchers in diverse fields including geomechanics, hydrogeology, wellbore integrity, geophysics, reservoir simulation, geochemical modeling, and risk assessment among others. The model is being refined to integrate additional wells and additional geological units not included in the Phase I model, including: 1) an “altered zone” of anhydrite and dolostone at the updip edge of the Weyburn–Midale reservoir that forms the caprock to the reservoir subjacent the regional seal formed by the Watrous Formation; and 2) a variably thick anhydrite unit, the Frobisher Evaporite, present at the base of the reservoir beneath the northern portion of the field. Both the altered zone and Frobisher Evaporite have been added to the model to improve characterization of long-term fluid behaviour in the Mississippian aquifers. Hydrogeological mapping in the Final Phase will include additional hydrogeological data. In Phase 1 of the project straddle pressure tests (those testing across multiple aquifers) were ignored because of their questionable applicability for individual aquifer characterization, and issues of aquifer assignment. These previously omitted samples are being integrated into the geocelluar model and used to further understand the fate of injected CO2 in key Mississippian aquifers (Midale, Frobisher and Ratcliffe). Investigating such straddle tests permits better evaluation of the possibility of cross-formational flow between the Mississippian aquifers, and the competency of inter- and intra- aquifer evaporites as potential barriers for CO2 migration. This paper will demonstrate the utility of using a geocellular model as a method of integrating data from diverse research interests on an evolving basis while maintaining an updated status with researcher accessibility. Integration of new geological and hydrogeological data into the model of the Weyburn Midale pool and surrounding area will provide the basis for much of the research ongoing in this project and for the simulation of long-term CO2 movement.

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: Simulation or modeling · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.266
Threshold uncertainty score0.347

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 head0.037
GPT teacher head0.286
Teacher spread0.248 · 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 designSimulation or modeling
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

Citations7
Published2009
Admission routes2
Has abstractyes

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