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Record W4250480427 · doi:10.1017/cbo9781316543832.001

Preface

2016· book-chapter· en· W4250480427 on OpenAlexaff
A. P. S. Selvadurai, A. P. Suvorov

Bibliographic record

VenueCambridge University Press eBooks · 2016
Typebook-chapter
Languageen
FieldEnvironmental Science
TopicLandslides and related hazards
Canadian institutionsMcGill University
Fundersnot available
KeywordsPorous mediumGeothermal gradientGeotechnical engineeringFluid dynamicsPoromechanicsGeologyHeat transferCreepAnisotropySlip (aerodynamics)MechanicsPorosityPetroleum engineeringMaterials scienceGeophysicsThermodynamicsPhysics

Abstract

fetched live from OpenAlex

Investigations of multiphysical processes in geomaterials have come to the forefront due to the continuing interests in the application of such theories for solving complex geoenvironmental problems. The topic of geologic disposal of heat-emitting nuclear fuel requires the consideration of the simultaneous influences of mechanical deformations, fluid flow, heat transfer and chemical alterations. Similar processes are encountered in the geologic sequestration of greenhouse gases in fluidized forms, the extraction of geothermal energy from both shallow and deep sources, the fluid pressure-induced influences of faults during slip at a fault or rock fracture, the mechanics of frozen soils, and geomechanical influences of glacial advances. The complete consideration of all possible multiphysical interactions in geomaterials is a daunting task and clearly an unrealistic expectation. For example, the study of thermo-hydro-mechanical effects in geologic media has to consider the mechanics of typical porous skeletons due to elastic, plastic and creep behavior, the fluid transport characteristics of the intact skeleton, and how these processes in turn can be influenced by the mechanical alterations of the porous skeleton and the heat transfer processes. In addition, chemical actions can alter the mechanical, fluid flow and thermal properties of the geological medium. The coupled multiphysical influences can be made more complicated by introducing considerations such as anisotropy, heterogeneity of the porous fabric and non-saturation of the porous medium. Clearly, the consideration of all these processes is formidable when the constitutive functionals and parameters have to be determined experimentally to make the results meaningful for geoscientific applications. The situation becomes even more complex because the interpretation of material data gathered for geoscientific applications can vary from the laboratory miniature specimen scale through the bench scale to the field scale. The prudent approach is to keep the multiphysical interactions to a bare minimum so that the processes that are critical to geoscientific applications can be emphasized. Such an approach requires a great deal of experience and patience. Although this volume largely focuses on geomaterial behavior, the range of applications of the theories of thermo-poroelastic behavior extends beyond the geosciences and can provide useful approaches to modeling problems in diverse areas, from biomechanics, notably the mechanics of bone materials and soft tissues, to industrial processes, involving drying of porous materials.

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)0.006
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: Other · Consensus signal: Other
Teacher disagreement score0.657
Threshold uncertainty score0.000

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0010.006
Meta-epidemiology (narrow)0.0010.000
Meta-epidemiology (broad)0.0010.001
Bibliometrics0.0020.002
Science and technology studies0.0020.001
Scholarly communication0.0040.003
Open science0.0010.003
Research integrity0.0020.002
Insufficient payload (model declined to judge)0.6570.489

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 head0.011
GPT teacher head0.172
Teacher spread0.162 · 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
GenreOther

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
Published2016
Admission routes1
Has abstractyes

Explore more

Same venueCambridge University Press eBooks→Same topicLandslides and related hazards→French-language works237,207→