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Record W2054505933 · doi:10.1139/l07-103

Reply to the discussion by H. Chanson and L. Toombes on "Characteristics of free overfall for supercritical flows"

2007· article· en· W2054505933 on OpenAlexvenueno aff
Nuray Denli Tokyay

Bibliographic record

VenueCanadian Journal of Civil Engineering · 2007
Typearticle
Languageen
FieldEngineering
TopicFluid Dynamics and Turbulent Flows
Canadian institutionsnot available
Fundersnot available
KeywordsSupercritical fluidSupercritical flowThermodynamicsPhysicsMechanicsStatistical physicsMathematics

Abstract

fetched live from OpenAlex

We thank the discussers for their interest in our paper. It is stated in our paper that the downstream position of the drop for a supercritical flow has not been investigated. Chanson and Toombes (1998) published a paper entitled “Supercritical flow at an abrupt drop: flow patterns and aeration”, and we are sorry that we missed this paper when conducting our literature review. However, after reviewing their study, it was found that there are major differences between the present study and the study of the discussers. The discussers state that “the supercritical flow at an abrupt drop is strongly three-dimensional and unsteady, and this aspect has direct implications for engineering designs.” In several sections of our paper, it is emphasized that the flow at an abrupt drop is strongly three-dimensional (see p. 163). However, as long as the inflow discharge remains constant, the average behavior of flow should be steady. In our case the flow was steady. Another difference is the upstream boundary condition. In our study, the supercritical flow before the drop was generated by a sluice gate. In the discussers’ study, however, the supercritical flow was generated by an elliptical convergent nozzle. Chanson and Toombes (1998) claim that the approach flow and the free-falling nappe were basically twodimensional, and at the downstream of the nappe impact the flow became three-dimensional. In our case, as explained on p. 164 under the subtitle “Characteristics of the base of the free overfall”, it was observed that the jet leaving the drop showed a horizontal and vertical spread due to variation of velocity across the cross section of the channel. The streamlines near the center had higher velocities than those near the sidewalls, therefore the streamlines leaving the drop near the sidewalls hit the base channel at a distance shorter than those near the centerline, resulting in a three-dimensional jet. The discussers claim that “for all experiments, nappe ventilation was provided at the first drop by sidewall splitters.” In their paper (Chanson and Toombes 1998), however, they stated that “the study presents new experimental data obtained in a 0.5 m wide stepped flume with an unventilated nappe”, which is a contradiction to the statement in their discussion. Another claim of the discussers is that “At the nappe impact, the change in flow direction on the invert resulted in the formation of sidewall standing waves and shockwaves in the downstream supercritical flow.” In our study, we never observed a sidewall standing wave. It was observed that at the base of the supercritical free overfall, a heavy splash of water takes place at a small Froude number and vigorous mixing and turbulence takes place at the end of the jet. As the Froude number of the upstream flow increases, this heavy splash takes the form of a standing wave that has a maximum height at the centerline of the channel. The discussers relate the properties they have observed at the base of the free overfall to a downstream ideal flow Froude number, Fr. However, a supercritical flow is subject to an upstream control. This seems to be a significant contradiction to the nature of the supercritical flow. If Chanson and Toombes (1998) used side splitters to aerate the nappe, it may have caused the sidewall standing waves. Yet, they claim that the falling jet is a two-dimensional jet; this may also cause a sidewall standing wave. In our case, the falling jet was a three-dimensional jet. Experimental observations showed that water accumulates behind the jet as in the case of subcritical flow free fall. They do not mention the phenomenon of standing water behind the jet. It seems to us that the sidewall standing wave generated in the discussers’ study is a type of standing water behind the jet that was influenced by upstream conditions. The discussers also state that “Downstream of the nappe impact, flow was characterized by a highly fragmented spray. The spray and splashing appeared to be concentrated towards the centerline of the channel”, which was also discussed in our paper in the subsection entitled “Characteristics of the base of the free overfall”. As expressed in subsection “Depth of flow y2” of our paper, the flow was also supercritical in the downstream channel. It is the nature of supercritical flow that cross waves occur because of changes in direction, and this is also mentioned in several places in the text.

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.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.012
metaresearch head score (Gemma)0.052
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Not applicable · Consensus signal: Not applicable
GenreCandidate signal: Commentary · Consensus signal: Commentary
Teacher disagreement score0.052
Threshold uncertainty score0.064

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0120.052
Meta-epidemiology (narrow)0.0020.002
Meta-epidemiology (broad)0.0030.003
Bibliometrics0.0020.002
Science and technology studies0.0060.008
Scholarly communication0.0060.014
Open science0.0090.006
Research integrity0.0520.071
Insufficient payload (model declined to judge)0.0070.006

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 head0.005
GPT teacher head0.181
Teacher spread0.176 · 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 source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designNot applicable
Domainnot available
GenreCommentary

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
Published2007
Admission routes1
Has abstractyes

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