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Record W1989482214 · doi:10.2118/2004-213

Effect of Hysterisis on Flow in Porous Media

2004· article· en· W1989482214 on OpenAlexaff
L.B. Cunha, E. J. Bonet

Bibliographic record

VenueCanadian International Petroleum Conference · 2004
Typearticle
Languageen
FieldEngineering
TopicHeat and Mass Transfer in Porous Media
Canadian institutionsUniversity of Alberta
Fundersnot available
KeywordsPorous mediumFlow (mathematics)Materials sciencePorosityPetroleum engineeringMechanicsComposite materialEngineeringPhysics

Abstract

fetched live from OpenAlex

Abstract The hysterisis phenomenon affects the flow behaviour in various occasions. In particular, during the WAG process the cyclic injections of wetting and non-wetting (water and gas) fluids cause the appearance of the hysterisis phenomena. In this work, to access the magnitude of the hysterisis phenomena on the flow in porous media we performed experimental tests and analytical studies. We measured for different formations the relative permeabilities in the imbibition and drainage cycle, using oil and water. We monitored the rates and pressures at the inlet and outlet points of the rock sample and also the internal saturation evolution. These data permitted to obtain the fractional flow curve for the associated imbibition and drainage processes. We then performed a flow test, which result, could be compared with different mathematical approaches proposed in the literature to take into account the effect of hysterisis on flow in porous media. There are in the literature different proposals to calculate the flow in porous media honouring the hysteretic flow. We used three semi-analytical and one numerical method to describe the experimental test. At the end, a comparison between the results obtained is presented. Introduction The hysterisis phenomena in flow in porous media manifest itself in different occasions. In the oil exploitation we could mention the cyclic injection of gas and water for the WAG process, in the ascending and descending of the water cone, in the gas injection and production of storage aquifers, in the miscellar flooding process where an oil bank is displaced by water(1)(2)(3)(4)(5)(6). In hydrology the ascending and descending of the water table in the vadoze zone presents a hysterisis phenomena (7). Different rocks and fluids present different degrees of hysterisis. It is believed that this phenomena depends on, besides fluid properties, morphological and topological aspects of porous media (8). Normally the hysterisis manifests itself in different petrophysical properties. The more frequently cited in the literature are the capillary pressure, fractional flow curves and relative permeabilities. The first drainage presents a very pronounced hysterisis. In oil fields, normally the first drainage occurs in the secondary oil migration and is not present in the exploitation stage. For this reason we will not consider it in this article and only periods after the first imbibition and secondary drainage will be considered. In our paper we will focus mainly on the two-phase relative permeabilities, and its derived fractional flow curve. The main reason for not measuring capillary hysterisis is the fact that semi-analytical models based on hyperbolic equation based on mass conservation do not consider the capillary pressure. Also, the literature shows that this is an acceptable simplification. For our two-phase system there is some controversy about the behaviour of different curves. Our experimental results confirm, what is usually acceptable, that the hysterisis effect is important only on the non-wetting phase permeability and the imbibition permeability is greater than the drainage (3)(9)(10)(11). We measured the relative permeability in a steady-state process and calculated and compared experimental tests with one numerical and three semi-analytical methods (12)(13)(14)(15)(10)(11)(16)(17(18).

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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: Simulation or modeling · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.571
Threshold uncertainty score0.993

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 head0.008
GPT teacher head0.214
Teacher spread0.206 · 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 designSimulation or modeling
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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Citations0
Published2004
Admission routes1
Has abstractyes

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