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Record W4392760195 · doi:10.5194/egusphere-egu24-12878

Feasibility of in-situ carbon mineralization in serpentinite via shallow injection, British Columbia, Canada

2024· preprint· en· W4392760195 on OpenAlexaffabout
Katrin Steinthorsdottir, Greg Dipple, Sandra Ó. Snæbjörnsdóttir, Mana Rahimi, Shandin Pete, Christa Pellett, Brady Clift, Salka Kolbeinsdóttir

Bibliographic record

Venuenot available
Typepreprint
Languageen
FieldComputer Science
TopicGeochemistry and Geologic Mapping
Canadian institutionsGeoscience BCUniversity of British Columbia
Fundersnot available
KeywordsMineralization (soil science)In situGeologyGeochemistryCarbon fibersMining engineeringChemistrySoil scienceMaterials science

Abstract

fetched live from OpenAlex

Carbon storage via shallow CO2 injection and mineralization in subsurface geologic formations has been demonstrated at the kilotonne scale in basalt (e.g., Hellisheidi, Iceland) but not in ultramafic rock. This type of storage dissolves CO2 in water that is then injected underground into shallow rock formations from 300-2000 m depth, where it reacts and forms permanent carbonate minerals. This project assesses the potential for CO2 injection into serpentinite, specifically within British Columbia, Canada.Site selection included multi-criteria index overlay analysis for logistical factors (e.g. water, electricity, access) and evaluation of geological data to prioritize which sites contain 1 km2 mapped voluminous serpentinite. Of the 746 mapped ultramafic formations, 84 formations within 21 areas meet threshold criteria, and of these, three stand out with clearly higher potential. These are 1) the Shulaps complex, 2) the Coquihalla serpentine belt, and 3) the Tulameen intrusion, all in southwest British Columbia. These areas have in common that they are close to infrastructure, are located in regions with higher annual temperatures, and have known geological and geophysical characteristics indicative of serpentinite. The Shulaps and Coquihalla are mantle massifs and mainly composed of serpentinized harzburgite, and Tulameen is an Alaskan-type ultramafic intrusion with a serpentinized dunite core.Six different carbon storage potential estimates using volume limitations, dissolution, and reactivity rates from experiments, and natural analogues are shown for the three potential sites, for Shulaps 141.2-18,682 MtCO2, for Coquihalla 9.416-1,245 MtCO2, and for Tulameen 2.825-373.6 MtCO2. Fieldwork observations and preliminary results show, as expected, heterogeneity of protoliths, serpentinization extent, and fracture density between the areas. Coquihalla was selected for a proposed pilot injection study because of its high serpentinization extent (>90%, suggesting high reactivity), continuous high fracture density (suggesting adequate injectivity), site accessibility through existing road systems, and proximity to electricity.An additional aspect of project development is engagement with local communities. All three of the top-ranked sites fall within traditional lands of First Nations peoples, and we conducted early engagement with 22 First Nations or alliances. The priorities for engagement were to inform people about the project and its implications, get consent for fieldwork, have a discussion, and start relationship building.

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 machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.023
Threshold uncertainty score0.093

Distilled classifier scores by category (both heads)

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

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 head0.013
GPT teacher head0.218
Teacher spread0.205 · 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 source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
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

Citations1
Published2024
Admission routes2
Has abstractyes

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