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Record W1543900729 · doi:10.5772/15126

Evolution of Ripple Field Architecture during Sediment Transport, as Measured by CT Scanning

2011· book-chapter· en· W1543900729 on OpenAlexaff
Long Bernard, Montreuil Stephane

Bibliographic record

VenueInTech eBooks · 2011
Typebook-chapter
Languageen
FieldEnvironmental Science
TopicHydrology and Sediment Transport Processes
Canadian institutionsInstitut National de la Recherche Scientifique
Fundersnot available
KeywordsRippleSediment transportFlumeSedimentGeologyGeomorphologyRipple marksBedformFlow (mathematics)Hydrology (agriculture)Geotechnical engineeringEngineeringMechanicsPhysics

Abstract

fetched live from OpenAlex

Despite the advent of ever more sophisticated technologies, the study of sediment transport remains highly relevant.Ongoing climate change adds urgency to the need to understand phenomena governing sediment transport.During sediment movement, the architecture of the sediment bed evolves (Nummedal et al., 1993;Allen and Posamentier, 1994;Van Wagoner, 1995).This chapter focuses on the fundamental processes involved in sediment transport and aims to define and characterize the evolution of the water-sediment mixture in a migrating sand ripple field under a stationary flow regime, from the flow surface to the base of the sediment bed.In an experimental sediment flume with attached computed tomography (CT)-scanner, the sediment density of a ripple field was studied at different phases of its architectural evolution using three-and four-dimensional X-ray scanning, under several flow regimes and with different grain sizes.This approach yielded a detailed understanding of the parameters involved in transport of sand-grade sediment. MethodsThis study used two hydraulic flumes.One was a vertical, closed-loop flume 3048 mm long and 1219 mm high designed by Teeter and Pankow (1989).The inner rectangular section of the flume (152 mm by 304 mm) passed through the mobile gantry of a computed tomography (CT)-scanner.The lower part of the tunnel was partly filled with a 30 mm-thick layer of C-109 Ottawa sand (0.37 mm grain size, with bulk dry density of 1.56 g•cm -³).The flow regime was adjusted by an electrical motor to 25 cm•s -1 and controlled by a Doppler flow meter (Controlotron 1010N).For more details of this apparatus, see Montreuil (2006).In this flume experiment, the volume element (voxel) chosen was 0.39 mm by 0.60 mm by 1.00 mm.Typical density profiles along the ripple bed were extracted from the CT-scanner measurement matrix of 512 x 512 x 512 voxels and a 305 x 305 x 200 mm volume.The second flume was an open acrylic flume (300 x 300 x 7000 mm) looped by a pump with 1.51 m 3 •min -1 capacity.The rectangular section of the flume (300 x 300 mm), passed through the mobile gantry of the CT-scanner (Fig. 1).The steady flow, measured by a Controlotron www.intechopen.com

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)0.000
metaresearch head score (Gemma)0.000
Version: metacan-v3-hybrid-931329e0061cValidation 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 score0.002
Threshold uncertainty score0.004

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0010.000

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 head0.010
GPT teacher head0.197
Teacher spread0.188 · 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 designObservational
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

Citations2
Published2011
Admission routes1
Has abstractyes

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