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The three effects of the pressure force on turbulent boundary layers

2025· article· en· W4411544588 on OpenAlexafffund
Taygun R. Gungor, Ayse G. Gungor, Yvan Maciel

Bibliographic record

VenueInternational Journal of Heat and Fluid Flow · 2025
Typearticle
Languageen
FieldEngineering
TopicFluid Dynamics and Turbulent Flows
Canadian institutionsUniversité Laval
FundersNatural Sciences and Engineering Research Council of CanadaAlliance de recherche numérique du CanadaPartnership for Advanced Computing in Europe AISBL
KeywordsTurbulenceMechanicsBoundary layerFlow separationMaterials scienceBoundary layer thicknessBoundary (topology)Classical mechanicsPhysicsMathematicsMathematical analysis

Abstract

fetched live from OpenAlex

This study aims to isolate the three effects of the pressure force on the inner and outer layers: the local direct impact (characterized by the pressure gradient parameter, β ), the local disequilibrating effect (represented here by the normalized streamwise derivative d β / d X ), and the upstream cumulative effect, while also accounting for the inevitable Reynolds number influence. To achieve this objective, we draw on several non-equilibrium and near-equilibrium databases from the literature, and employ a methodology based on the selection of pressure-gradient parameters — distinct for the inner and outer layers — that capture the local direct impact and the local disequilibration effect of the pressure gradient. The pressure force impact on the inner and outer regions is represented by two parameters: the friction–viscous pressure-gradient parameter, β i , and the pressure-gradient parameter based on Zagarola–Smits velocity, β Z S , respectively. In the non-equilibrium flow cases, both β i and β Z S exhibit similar distributions, initially increasing and then decreasing. However, the rate of change of these parameters along the streamwise direction varies among the flows, indicating differing levels of pressure force disequilibration. In addition, we employ two near-equilibrium cases with minimal variations of the pressure gradient parameters for comparisons. In the outer layer, it is found that both the local and cumulative disequilibrating effects modify the mean velocity and Reynolds stress profiles at identical β Z S values. The faster the variations in pressure force impact, the more delayed the response of both mean flow and turbulence. Cumulative effects prove to be significant. In the inner layer, which responds much faster to changes in pressure force, the local disequilibrating effect still modifies the mean velocity profile in the viscous sublayer. Notably, when the mean velocity defect is significant, the behavior of u -structures in the inner layer appears to be governed by how outer turbulence responds to pressure force effects. In contrast, the size of u v -structures in the inner layer scales with the mixed pressure-friction length ( ν / u τ + ν / u p i ) . Unlike inner u -structures, they are independent of large-scale outer structures and flow history. • Pressure force variations alter the flow even when the force balance is similar. • Rapid pressure force variations further delay the flow response. • Flow history has minimal effect on inner velocity, regardless of pressure force. • Inner-layer u v -structures size scales with a mixed friction–pressure length scale.

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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: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.119
Threshold uncertainty score0.205

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 head0.003
GPT teacher head0.201
Teacher spread0.198 · 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".

Quick stats

Citations0
Published2025
Admission routes2
Has abstractyes

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