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Enregistrement W2099802774 · doi:10.2113/gscpgbull.59.3.235

Horseshoe Canyon and Belly River coal measures, south central Alberta: Part 2 -- Modeling reservoir properties and producible gas

2011· article· en· W2099802774 sur OpenAlex
A. M. M. Bustin, R.M. Bustin, J. Russel-Houston

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affAu moins un auteur déclare une institution canadienne dans l'instantané OpenAlex épinglé.
venuePublié dans une revue dont le pays d'attache est le Canada.
aboutLe titre ou le résumé porte un signal canadien du lexique géographique.

Notice bibliographique

RevueBulletin of Canadian Petroleum Geology · 2011
Typearticle
Langueen
DomaineEngineering
ThématiqueCoal Properties and Utilization
Établissements canadiensUniversity of British Columbia
Organismes subventionnairesnon disponible
Mots-clésCanyonGeologyArchaeologyCitationMining engineeringPetroleumLibrary scienceGeographyPaleontologyGeomorphology

Résumé

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Research Article| September 01, 2011 Horseshoe Canyon and Belly River coal measures, south central Alberta: Part 2 — Modeling reservoir properties and producible gas A.M.M. Bustin; A.M.M. Bustin The University of British Columbia, 6339 Stores Road, Vancouver, BC V6T 1Z4, abustin@eos.ubc.ca Search for other works by this author on: GSW Google Scholar R.M. Bustin R.M. Bustin The University of British Columbia, 6339 Stores Road, Vancouver, BC V6T 1Z4, bustin@mail.ubc.ca Search for other works by this author on: GSW Google Scholar Author and Article Information A.M.M. Bustin The University of British Columbia, 6339 Stores Road, Vancouver, BC V6T 1Z4, abustin@eos.ubc.ca R.M. Bustin The University of British Columbia, 6339 Stores Road, Vancouver, BC V6T 1Z4, bustin@mail.ubc.ca Publisher: Canadian Society of Petroleum Geologists Received: 08 Apr 2011 Accepted: 12 Sep 2011 First Online: 13 Jul 2017 Online Issn: 2368-0261 Print Issn: 0007-4802 © the Society of Canadian Petroleum Geologists Bulletin of Canadian Petroleum Geology (2011) 59 (3): 235–260. https://doi.org/10.2113/gscpgbull.59.3.235 Article history Received: 08 Apr 2011 Accepted: 12 Sep 2011 First Online: 13 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation A.M.M. Bustin, R.M. Bustin; Horseshoe Canyon and Belly River coal measures, south central Alberta: Part 2 — Modeling reservoir properties and producible gas. Bulletin of Canadian Petroleum Geology 2011;; 59 (3): 235–260. doi: https://doi.org/10.2113/gscpgbull.59.3.235 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyBulletin of Canadian Petroleum Geology Search Advanced Search Abstract The gas reserves and well spacing units in the Horseshoe Canyon-Belly River Formation coal measures in Alberta are assigned based on gas-in-place determined by canister desorption tests of coal following ERCB (2010) guidelines. However, substantial gas, which is not measured by desorption tests, also occurs in the free state within the coals as well as adsorbed and in the free state within adjacent fine-grained strata (referred to here as shales) interbedded with the coals. A series of laboratory experiments (matrix flux, volumetric strain, rock mechanics) were conducted to quantify the reservoir properties of the coals and shales and were integrated with the results from field tests (well logs, pressure build-up) to be used as model inputs for a reservoir simulator. The purpose of the modeling was to address two main questions: 1) do variations in the amount of free gas within the matrix porosity of the coal seams affect production; and 2) to what extent is the gas stored within the strata interbedded with the coal seams co-produced?The free gas stored within a coal seam with an effective matrix porosity of 8% is shown to comprise on the order of 25% of the total original gas-in-place. The modeling results show that in high permeability coals (150 mD), an increase in production equivalent to the additional gas-in-place resulting from the free gas occurs after 25 years. Even very low permeability reservoirs (0.3 mD) are modeled to experience an approximately 2% increase in cumulative gas after 50 years of production.Including the gas bearing shales adjacent to the coal seams results in a substantial increase in producible gas. An increase of 144% in the cumulative gas produced after 50 years is observed when shales with a fracture permeability of 0.01 mD, matrix permeability of 1×10−4 mD, and an effective fracture spacing of 10 m are modeled with coal seams with a fracture permeability of 15 mD. The coal seams, being more permeable than the shales, act as horizontal drains for the over and underlying shale layers. The enhanced production is strongly dependent on the fracture and matrix permeability as well as the fracture spacing of the shales. The spacing of 4 wells/section, assumed in the above model, results in an estimated ultimate recovery (EUR) of 23% of the total original gas-in-place in the coals and 9% in the shales after 50 years of production. Downsizing to 8 wells/section increases the EUR to 35% for the coals and 15% for the shales and to 16 wells/section to 50% for the coals and 22% for the shales. The resulting increase in cumulative production with the decrease to 8 wells/section spacing is 57% and an additional 42% when further decreased to 16 wells/section. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Récupéré en direct depuis OpenAlex et désinversé. Les résumés ne sont pas conservés dans cette base de données : les index inversés représentent 8,6 Go des 9,3 Go de texte de la base, et le serveur dispose de 13 Go libres.

Prédiction distillée sur la base complète

Imitation des enseignants

Ni prévalence calibrée, ni vérité terrain. Validation humaine à venir. Apprise à partir de 10 348 étiquettes directes de Codex et de 10 348 étiquettes directes de Gemma. Le mode candidate est l'union des têtes enseignantes seuillées; le consensus est leur intersection. Ces sorties portent le statut machine_predicted_unvalidated et ne sont ni des étiquettes humaines ni des étiquettes directes de modèles de pointe.

score de la tête « metaresearch » (Codex)0,000
score de la tête « metaresearch » (Gemma)0,000
Version: codex-gemma-dda1882f352aStatut de validation: machine_predicted_unvalidated
Catégories candidatesaucune
Catégories consensuellesaucune
DomaineSignal candidat: aucune · Signal consensuel: aucune
Devis d'étudeSignal candidat: Sans objet · Signal consensuel: aucune
GenreSignal candidat: Empirique · Signal consensuel: Empirique
Score de désaccord entre enseignants0,672
Score d'incertitude au seuil0,693

Scores Codex et Gemma par catégorie

CatégorieCodexGemma
Métarecherche0,0000,000
Méta-épidémiologie (sens strict)0,0000,000
Méta-épidémiologie (sens large)0,0000,000
Bibliométrie0,0000,000
Études des sciences et des technologies0,0000,000
Communication savante0,0000,000
Science ouverte0,0000,000
Intégrité de la recherche0,0000,000
Charge utile insuffisante (le modèle a refusé de juger)0,0000,000

Scores machine (provisoires)

Les deux têtes enseignantes du modèle étudiant, lues sur ce travail. Un score ordonne la base pour la relecture; il n'affirme jamais une catégorie, et le statut de validation accompagne chaque rangée tel quel.

Scores de référence d'un modèle non mature (critères de maturité non atteints, 7 itérations). Un score ordonne; il n'affirme jamais une catégorie.

Tête enseignante Opus0,036
Tête enseignante GPT0,160
Écart entre enseignants0,124 · la distance entre les deux têtes enseignantes sur ce seul travail
Statut de validationscore_only:v0-immature-baseline · tel quel depuis la passe de notation : score_only signifie que le nombre peut ordonner les travaux, et qu'aucune étiquette de catégorie n'en découle