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Record W2239024882 · doi:10.1021/acs.jpcc.5b09683

Molecular Understanding of CO<sub>2</sub> and H<sub>2</sub>O in a Montmorillonite Clay Interlayer under CO<sub>2</sub> Geological Sequestration Conditions

2016· article· en· W2239024882 on OpenAlexfundno aff
Qi Rao, Yongsheng Leng

Bibliographic record

VenueThe Journal of Physical Chemistry C · 2016
Typearticle
Languageen
FieldEnvironmental Science
TopicCO2 Sequestration and Geologic Interactions
Canadian institutionsnot available
FundersNatural Sciences and Engineering Research Council of CanadaAmerican Chemical Society Petroleum Research Fund
KeywordsMontmorilloniteClay mineralsCarbon sequestrationGeologyGeochemistryMineralogyChemistryCarbon dioxideOrganic chemistry

Abstract

fetched live from OpenAlex

Grand canonical Monte Carlo (GCMC) simulations are carried out to investigate a supercritical carbon dioxide (scCO 2 )-water mixture in the Na-montmorillonite clay interlayer under typical CO 2 geological sequestration conditions ( T = 323 K, P = 90 bar and T = 348 K, P = 130 bar). The stable clay interlayer distances at different relative humidity (RH) are determined based on the normal pressure and free energy curves of the CO 2 –H 2 O–Na + complex in the montmorillonite clay interlayer. Simulation results show that stable monolayer hydrates (1W) with a basal spacing around 12 Å are formed at RH = 30–60%. As RH is increased to 70% and above, bilayer CO 2 –H 2 O mixtures with a basal spacing around 15–16 Å (2W) are more stable. In general, the CO 2 intercalation process is strongly influenced by RH. While a high relative humidity facilitates water molecules entering the clay interlayer, it nonetheless decreases CO 2 intercalations. The sorbed H 2 O concentrations from our simulations compare remarkably well with the in situ infrared (IR) spectroscopy experimental data by Loring et al. [ Langmuir, 2014, 30, 6120–6128], if the continuous experimental curve is considered as the “smear-out” of the stepwise curve from our simulations. However, the overall sorbed CO 2 concentrations from our simulations are higher than the IR experimental results. We attribute these discrepancies in both sorbed H 2 O and CO 2 concentrations (measured from experiments and simulations) to the complexity of hydrated clay particles in the IR spectroscopy experiment, to which the hydration-heterogeneity model could provide a reasonable interpretation. Molecular dynamics (MD) simulations show that the hydration state of CO 2 molecules is changed from the partial hydration in 1W to the full hydration in 2W with the increase in RH, and CO 2 dimers are frequently seen in both 1W and 2W hydration states. CO 2 dimers largely take the slipped parallel configurations, while the remaining dimers take the perpendicular T-shaped geometry. Further, sodium ions in the interlayer tend to be fully hydrated by water molecules due to their relatively large hydration energy. Moreover, we find that CO 2 molecules hardly migrate into the first hydration shell of sodium ions. The overall diffusion coefficients of CO 2 molecules are larger than those of water molecules and sodium ions. This comparably high mobility of CO 2 molecules in the clay interlayer, together with the low probability of CO 2 participation in the first hydration shell of Na + ions, essentially prevents CO 2 and Na + from direct interactions in clay interlayers.

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 score0.016
Threshold uncertainty score0.694

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 studies0.0000.001
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 head0.019
GPT teacher head0.266
Teacher spread0.247 · 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

Citations55
Published2016
Admission routes1
Has abstractyes

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