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Record W1972425597 · doi:10.2118/149223-ms

A New Unified Diffusion-Viscous Flow Model Based on Pore Level Studies of Tight Gas Formations

2011· article· en· W1972425597 on OpenAlex

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.

affAt least one author lists a Canadian institution in the pinned OpenAlex snapshot.
aboutThe title or abstract carries a Canadian signal from the geographic lexicon.

Bibliographic record

VenueCanadian Unconventional Resources Conference · 2011
Typearticle
Languageen
FieldEngineering
TopicHydrocarbon exploration and reservoir analysis
Canadian institutionsUniversity of Calgary
Fundersnot available
KeywordsPorous mediumTight gasPermeability (electromagnetism)Flow (mathematics)MechanicsHele-Shaw flowFluid dynamicsSlippageIsothermal flowComputer scienceGeologyPorosityGeotechnical engineeringMaterials scienceOpen-channel flowPhysicsChemistry

Abstract

fetched live from OpenAlex

Abstract A new technique for numerical reconstruction of porous media is proposed that combines the flexibility and easy data conditioning of pixel-based multiple point statistics (MPS) along with robustness of object-base algorithms. Single phase gas flow simulations that consider slippage effects through a network of slots and micro-fractures extracted from petrographic work in tight porous media of the Nikanassin Group in the Western Canada Sedimentary Basin (WCSB) have been conducted. Furthermore, correlations between Klinkenberg slippage effect and absolute permeability have been developed. This leads to a new unified flow model in which Knudsen number acts implicitly as a flow regime indicator. A detailed understanding of fluid flow at the micro scale level in tight porous media is essential to establish and develop techniques for economic flow rate and recovery. Direct available imaging techniques cannot capture all the details of tight formations at the pore level. Choosing an appropriate equation for flow through a single element of the network is crucial; this equation must include geometry and other structural features that affect the flow as well as all variation of fluid properties with pressure. Disregarding these details in a single element of porous media can easily lead to flow misinterpretation at the macroscopic scale. Due to the wide flow-path-size distribution in tight porous media, a variety of flow regimes can exist in the equivalent network. Two distinct flow regimes, viscous flow and free molecular flow, are in either side of this flow regime spectrum. Since the nature of these two types of flow is categorically different, finding/adjusting a unified flow model is problematic. The complication stems from the fact that the viscosity concept misses its meaning as the flow regime changes from viscous to free molecular flow in which a diffusion-like flow mechanism dominates. For each specified flow regime, the appropriate equations for different geometries are studied. Also, different unified flow models available in the literature are critically investigated. Simulation of gas flow through the constructed network at different mean flow pressures leads to investigate the functionality of Klinkenberg factor with permeability of the porous media and pore-level structure. It is concluded that for tight formations the slippage effects is more pronounced and cannot be neglected in the flow equations.

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: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: none
Teacher disagreement score0.755
Threshold uncertainty score0.953

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)0.0010.000

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 head0.086
GPT teacher head0.243
Teacher spread0.157 · 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