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Record W4234045120 · doi:10.2523/77333-ms

Application of Leaky Aquifer Type Curves for Coalbed Methane Characterization

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

Bibliographic record

VenueProceedings of SPE Annual Technical Conference and Exhibition · 2002
Typearticle
Languageen
FieldEngineering
TopicHydraulic Fracturing and Reservoir Analysis
Canadian institutionsQuest University Canada
Fundersnot available
KeywordsAquiferCoalbed methanePetroleum engineeringGeologyGroundwaterMining engineeringEngineeringCoalGeotechnical engineeringWaste managementCoal mining

Abstract

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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.

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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 score0.104
Threshold uncertainty score0.352

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)0.0000.000

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 head0.018
GPT teacher head0.237
Teacher spread0.220 · 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".

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Citations2
Published2002
Admission routes1
Has abstractyes

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