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Record W7046302216

Determining rock erodibility parameter « relative block
\nstructure » for non-perpendicular hydraulic flow

2018· other· en· W7046302216 on OpenAlexfundno aff

Bibliographic record

VenueConstellation (Université du Québec à Chicoutimi) · 2018
Typeother
Languageen
FieldPhysics and Astronomy
TopicMagnetic confinement fusion research
Canadian institutionsnot available
FundersNatural Sciences and Engineering Research Council of CanadaMitacsHydro-Québec
KeywordsCompression (physics)Block (permutation group theory)Measure (data warehouse)Deformation (meteorology)
DOInot available

Abstract

fetched live from OpenAlex

The most commonly used method for assessing the hydraulic erodibility of rock is the Annandale’s method. This method is based on a correlation between the force of flowing water and the capacity of rock resistance. This capacity is evaluated using the Kirsten’s index which was initially developed to evaluate the excavatability of earth materials. This index is determined according to certain geomechanical factors, such as the compressive strength of intact rock, the rock block size, the discontinuities shear strength and the relative block structure. This last characteristic represents the required effort to erode the rock and, it can be quantified considering the shape and orientation of the blocks. To determine the relative rock structure in the field, the dip and dip direction of closer spaced joint set, as well as the ratio of joints spacingare required. It is found that the Kirsten’s concept can be applied only when the direction of flow is perpendicular to the strike of closer spaced joint set. Adjustments are introduced to Kirsten's initial concept concerning the relative block structure parameter. Thus, two equations are proposed which were used to propose a rating for the relative block structure parameter for a case example with non-perpendicular flow. \n \nLa méthode la plus utilisée en pratique pour l’évaluation de l’érodabilité hydraulique du roc est celle d’Annandale. Celle-ci se base sur une corrélation entre la force érosive de l’eau et la capacité de résistance du roc. Cette capacité est évaluée à l'aide de l’indice de Kirsten initialement développé pour évaluer l’excavabilité des matériaux. Cet indice est déterminé en fonction de certaines caractéristiques géomécaniques telles que la résistance matricielle de la roche intacte, la taille des blocs, la résistance au cisaillement des discontinuités et la structure relative des blocs. Cette dernière caractéristique représente l’effort requis pour que le roc soit érodé et, elle peut être quantifiée en considérant la forme et l’orientation des blocs. En pratique, elle se détermine en fonction du pendage et la direction du pendage de la famille des joints les moins espacés, ainsi que le ratio d’espacement des joints. Il est observé que le concept de Kirsten n’est valide que lorsque l’écoulement est perpendiculaire à l’azimut de la famille des joints les moins espacés. Des ajustements sont introduits sur le concept initial de Kirsten concernant la structure relative des blocs. Ainsi, deux équations sont proposées et utilisées pour générer des pondérations de la structure relative des blocs pour un exemple de cas avec un écoulement nonperpendiculaire.

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)0.001
metaresearch head score (Gemma)0.003
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Bench or experimental · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.003
Threshold uncertainty score0.011

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0010.003
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0020.001
Science and technology studies0.0000.000
Scholarly communication0.0010.001
Open science0.0010.001
Research integrity0.0010.000
Insufficient payload (model declined to judge)0.0030.001

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 head0.210
Teacher spread0.202 · 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 designBench or experimental
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
Published2018
Admission routes1
Has abstractyes

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