MétaCan
Menu
Back to cohort
Record W2325310871 · doi:10.1061/41016(314)300

Ice Forces on Inclined Bridge Piers

2008· article· en· W2325310871 on OpenAlexaboutno aff
Kenton W. Braun, Dempsey S. Thieman

Bibliographic record

VenueStructures Congress 2008 · 2008
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicArctic and Antarctic ice dynamics
Canadian institutionsnot available
Fundersnot available
KeywordsFlexural strengthBendingGeotechnical engineeringUltimate tensile strengthStructural engineeringCompressive strengthPure bendingMaterials scienceGeologyEngineeringComposite material

Abstract

fetched live from OpenAlex

The American Association of State and Highway Transportation Officials (AASHTO) and the Canadian Standards Association (CSA) codes provide design guidelines for determination of ice loads due to ice crushing and ice bending failures. Both organizations' bridge codes are based upon in-situ field measurements on two bridges in Alberta, Canada. Design formulas provided by both organizations (AASTHO and CSA) rely only on the effective crushing strength of ice to determine ice loading due to crushing failures and ice bending failures. Equations provided for bending failures rely on an assumed linear relationship between effective ice crushing strength and ice bending strength. Ice bending strength is apparently assumed to be 0.84 times the effective crushing strength using these codes. Recent in-situ testing of fresh water river ice on the North Slope of Alaska indicates that the ice bending strength is closer to 0.5 times the effective ice crushing strength for this location. Additionally, numerous studies have identified that ice crushing strength is highly dependent upon temperature, while ice bending strength remains relatively constant through changing temperatures. Results of the in-situ bending tests and other associated research indicate that calculations to determine ice forces due to bending failure should consider ice flexural or tensile strength rather than a direct correlation to effective ice crushing strengthen. This paper will present the testing methods and procedures, results and conclusions of flexural and compressive ice testing performed on river ice on the North Slope of Alaska. Comparisons between AASHTO and CSA predicted and actual bending strength will be made. An alternative calculation method determining the ice sheet bending strength will be presented. The authors recommend that the presented, alternative methods be adopted within the CSA and AASHTO codes to better predict ice loads associated with ice bending behavior.

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)0.001
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: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.008
Threshold uncertainty score0.028

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.001
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0000.001
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0080.002

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 head0.017
GPT teacher head0.228
Teacher spread0.211 · 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

Citations0
Published2008
Admission routes1
Has abstractyes

Explore more

Same venueStructures Congress 2008Same topicArctic and Antarctic ice dynamicsFrench-language works237,207