MétaCan
Menu
Retour à la cohorte
Enregistrement W4234045120 · doi:10.2523/77333-ms

Application of Leaky Aquifer Type Curves for Coalbed Methane Characterization

2002· article· en· W4234045120 sur OpenAlexaff
D.O. Cox, P.R. Onsager

Notice bibliographique

RevueProceedings of SPE Annual Technical Conference and Exhibition · 2002
Typearticle
Langueen
DomaineEngineering
ThématiqueHydraulic Fracturing and Reservoir Analysis
Établissements canadiensQuest University Canada
Organismes subventionnairesnon disponible
Mots-clésAquiferCoalbed methanePetroleum engineeringGeologyGroundwaterMining engineeringEngineeringCoalGeotechnical engineeringWaste managementCoal mining

Résumé

récupéré en direct d'OpenAlex

Application of Leaky Aquifer Type Curves for Coalbed Methane Characterization D.O. Cox; D.O. Cox Questa Engineering Corporation Search for other works by this author on: This Site Google Scholar P.R. Onsager P.R. Onsager Questa Engineering Corporation Search for other works by this author on: This Site Google Scholar Paper presented at the SPE Annual Technical Conference and Exhibition, San Antonio, Texas, September 2002. Paper Number: SPE-77333-MS https://doi.org/10.2118/77333-MS Published: September 29 2002 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Get Permissions Search Site Citation Cox, D.O., and P.R. Onsager. "Application of Leaky Aquifer Type Curves for Coalbed Methane Characterization." Paper presented at the SPE Annual Technical Conference and Exhibition, San Antonio, Texas, September 2002. doi: https://doi.org/10.2118/77333-MS Download citation file: Ris (Zotero) Reference Manager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex Search nav search search input Search input auto suggest search filter All ContentAll ProceedingsSociety of Petroleum Engineers (SPE)SPE Annual Technical Conference and Exhibition Search Advanced Search AbstractMany coalbed methane (CBM) reservoirs are part of larger aquifer units that also contain water-saturated sandstones. To account for connections to aquifers, this paper presents "leaky aquifer" type curves for radial flow in leaky aquifers with wellbore storage and skin, and for vertically fractured wells in leaky aquifers. The type curves are similar to those with a constant pressure boundary, and in some cases, the characteristic flat derivative of infinite-acting radial flow may be completely masked. Examples from several CBM basins are presented that demonstrate the methodology.IntroductionCoalbed methane (CBM) has developed into an important part of the U.S. gas supply over the last 20 years. In 1982, production from CBM reservoirs was virtually nonexistent, but recent tabulations show CBM reservoirs accounted for 7% of the total U.S. dry gas production and 9% of U.S. dry gas reserves in 20001.Coalbed methane reservoirs are considered unconventional gas reservoirs, for three main reasons2. First, in addition to being the reservoir rock, the coal is also the source rock for the gas in most cases. Secondly, the gas is stored by adsorption in the coal, rather than through the normal mechanism of compression by increased pressure. Finally, coal beds contain natural fractures, called cleats, which are commonly filled with water at the time the reservoir is discovered. For this reason, most CBM reservoirs require dewatering before they produce commercial volumes of gas.In some instances, water influx from other aquifer units can inhibit the dewatering of the coal and thereby limit coalbed methane recovery3. For this reason, methods to characterize the degree of connection between the coal and other units are needed.It has long been recognized in the groundwater industry that many aquifers have imperfect seals, and are in connection to other aquifer units through low permeability, "leaky" confining layers. In the late 1950's, Hantush and Jacob4,5, and Hantush6–8 published a series of papers with techniques to account for different boundary conditions and varying degrees of connection between aquifers. The Hantush-Jacob methodology is known in the groundwater industry as a "leaky aquifer" model. The idealized Hantush-Jacob leaky aquifer model of interest here is the one that assumed a constant pressure boundary at the top of the confining layer. This assumption is equivalent to having much greater horizontal permeability in the supporting aquifer than the vertical permeability of the confining layer. In 1969, Neuman and Witherspoon9 devised a more general model to account for finite permeability and volume in the aquifer providing pressure support.The leaky aquifer approach entered the petroleum literature for investigating the effectiveness of seals for gas storage projects in the 1960's and early 1970's10–12, but has had little use in the petroleum industry for pressure transient analysis. Instead, most of the petroleum-industry papers assume generalized multi-layer models with varying properties in each layer. Most of these papers consider well testing in layered formations with crossflow where all layers are open at the well13–17. In most cases with CBM wells, only the coal is producing, and the adjacent sandstone units that are in communication with the coal are commonly cased off. This type of boundary condition was considered in the general case with the properties of all layers being known by Witherspoon and Neuman12, Streltsova18, and Ehlig-Economides and Ayoub19. A recent paper by Guo, et al.20 considered either constant pressure or no-flow boundaries on the confining layer; this formulation is basically the same as that of Hantush and Jacob4. Keywords: application, radial flow, storage, leaky aquifer type curve, aquifer system, fractured well, coefficient, type curve, aquifer, leakance Subjects: Formation Evaluation & Management, Drillstem/well testing This content is only available via PDF. 2002. Society of Petroleum Engineers You can access this article if you purchase or spend a download.

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.

Comment cette classification a été obtenuedéplier

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: Expérimental (laboratoire) · Signal consensuel: Expérimental (laboratoire)
GenreSignal candidat: Empirique · Signal consensuel: Empirique
Score de désaccord entre enseignants0,104
Score d'incertitude au seuil0,352

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 Opus0,018
Tête enseignante GPT0,237
Écart entre enseignants0,220 · 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

Classification

machine, non validée

Prédiction automatique; un appel candidat d’une seule tête enseignante, pas un consensus.

Les modèles n’ont appliqué aucune catégorie : rien dans la taxonomie ne correspondait à ce travail.
Devis d'étudeExpérimental (laboratoire)
Domainenon disponible
GenreEmpirique

Le détail, modèle par modèle et score par score, se trouve en fin de page sous « Comment cette classification a été obtenue ».

En bref

Citations2
Publié2002
Routes d'admission1
Résumé présentoui

Explorer davantage

Même revueProceedings of SPE Annual Technical Conference and ExhibitionMême sujetHydraulic Fracturing and Reservoir AnalysisTravaux en français237 207