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Record W1590793182 · doi:10.21914/anziamj.v48i0.113

Natural convection flow in the cavity with isoflux boundaries

2008· article· en· W1590793182 on OpenAlex

Why this work is in the frame

A frame that forgets how it found something cannot be audited. These are the routes that admitted this work.

aboutThe title or abstract carries a Canadian signal from the geographic lexicon.
no affNo Canadian affiliation: this work is invisible to an affiliation-only frame.
No Canadian affiliation. An affiliation-only frame, the usual design, would never have seen this work. It is one of the works that make the case for inverting the frame.

Bibliographic record

VenueANZIAM Journal · 2008
Typearticle
Languageen
FieldEngineering
TopicNanofluid Flow and Heat Transfer
Canadian institutionsnot available
Fundersnot available
KeywordsNatural convectionMechanicsRayleigh numberAdiabatic processFinite volume methodConvectionPhysicsHeat transferHeat fluxThermodynamicsMaterials science

Abstract

fetched live from OpenAlex

Natural convection flow in rectangular cavities with uniform heat flux side walls and an adiabatic floor and ceiling is investigated. The analytical solution for the evenly heated and cooled infinitely tall cavity, obtained by integrating the energy equation over a certain control volume, is introduced and compared to a full numerical solution for the finite cavity. Numerical solutions have been obtained for cavities with height-to-width ratios of 1 to 10, various values of the heat flux and with parameters appropriate to both air and water. For high enough aspect ratio and/or Rayleigh number the numerical solutions at mid-height of the cavity and the cavity stratification are well predicted by the analytical solution for the infinite cavity. The flow on the cavity side walls is then one dimensional. References Armfeld, S. W., and Patterson, J. C., Direct simulation of wave interactions in unsteady natural convection in a cavity. Int. J. Heat Mass Transfer 34 (1991) 929--940. doi:10.1016/0017-9310(91)90004-X Armfeld, S. W., and Patterson, J. C., Wave properties of natural convection boundary layers. J. Fluid Mech. 239 (1992) 195--211. Desrayaud, G., and Nguyen, T. H., Instabilities themoconvectives dans une cavite a flux imposes, in Douzieme Congres Canadien de Mecanique Appliquee (1989) 716--717. Jiracheewanun, S., Armfield, S. W., Behnia, M., and McBain, G. D., The transient behaviour of a differentially heated cavity with isoflux boundaries, Proc. 15th A'asian Fluid Mechanics Conf. (2004) Paper AFMC00246. Kimura, S. and Bejan, A., The boundary layer natural convection regime in a rectangular cavity with uniform heat flux from the side, J. Heat Transfer 106 (No. 1) (1984) 98--103. Leonard, B. P., A stable and accurate convective modeling procedure based on quadratic upstream interpolation, Comp. methods appl. mech. engr. 19 (1979) 59--98. doi:10.1016/0045-7825(79)90034-3 Lietzke, A. F., Theoretical and experimental investigation of heat transfer by laminar natural convection between parallel plates, (NACA, 1955) Report 1223. McBain, G. D., Armfield, S. W. and Jiracheewanun, S., The conduction and convection regimes in a cavity with evenly heated and cooled vertical walls, 8th Australasian Heat and Mass Transfer Conf. (2005). (in press) Norris, S. E. and Armfield, S. W., Solving the Navier--Stokes equations on a workstation cluster, ANZIAM J. 42(E) (2000) C1058--C1075. http://anziamj.austms.org.au/V42/CTAC99/Norr Patterson, J. C. and Armfield, S. W., Transient features of natural convection in a cavity, J. Fluid Mech. 219 (1990) 469--497. Patterson, J. and Imberger, J., Unsteady natural convection in a rectangular cavity, J. Fluid Mech. 100 (1980) 65--86.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

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: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.262
Threshold uncertainty score0.259

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 integrity0.0000.001
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 head0.180
Teacher spread0.173 · 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