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Record W2550113039 · doi:10.1017/cbo9781316543832.005

Thermo-Poroelasticity of Geomaterial With a Fluid-Filled Rigid One-Dimensional Cavity

2016· book-chapter· en· W2550113039 on OpenAlexaff
A. P. S. Selvadurai, A. P. Suvorov

Bibliographic record

VenueCambridge University Press eBooks · 2016
Typebook-chapter
Languageen
FieldEngineering
TopicRock Mechanics and Modeling
Canadian institutionsMcGill University
Fundersnot available
KeywordsPoromechanicsPerpendicularStiffnessCavity wallMechanicsMaterials scienceDisplacement (psychology)Permeability (electromagnetism)GeologyPorosityPhysicsGeometryComposite materialPorous mediumMathematicsChemistry

Abstract

fetched live from OpenAlex

This chapter continues to examine the thermo-hydro-mechanical problems related to the one-dimensional case of deformation. The problem of a fluid-filled layer (cavity) bounded by two parallel planes is considered. This cavity is embedded into the center of a poroelastic region or body. Displacements, fluid and heat flow in this poroelastic region are allowed only in the direction perpendicular to the walls of the cavity. The elastic stiffness of the cavity is assumed to be very large compared to the stiffness of the surrounding poroelastic material and, consequently, the displacement of the cavity can only be due to thermal expansion of the solid material (skeleton) in the cavity. The problem has similarities to the classical hydraulic pulse tests developed by Brace et al. (1968) and Hsieh et al. (1981) and adopted widely for estimating the permeability characteristics of low-permeability geological materials (Selvadurai and Carnaffan, 1997; Butler, 1998; Selvadurai et al., 2005; Selvadurai et al., 2011; Selvadurai, 2009; Selvadurai and Jenner, 2012; Selvadurai and Ichikawa, 2013; Selvadurai and Najari, 2013, 2015; Najari and Selvadurai, 2014; Selvadurai and Selvadurai, 2014). An instantaneous pressure pulse or temperature change is applied to the volume of the cavity, and the evolution of the fluid pressure in the cavity with time is obtained. The rate of decay of the fluid pressure inside the cavity may allow us to estimate the permeability value of the surrounding poroelastic material. We present an analytical solution to this problem and compare the results with the finite element solution obtained using the ABAQUS™ finite element program. Problem of Fluid-Filled Rigid One-Dimensional Cavity: Formulation and Solution Assume that a fluid-filled rigid cavity (or a layer) occupying the region − a ≤ x ≤ a is embedded into a poroelastic geomaterial that occupies the region | x | > a (Fig. 4.1). A “rigid” cavity means that the elastic moduli of the cavity are significantly larger than those of the surrounding geomaterial. For example, the solid part of the cavity can be made of steel. The porosity of the cavity is assumed large, close to one, i.e., almost all the volume of the cavity is filled with fluid.

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: Simulation or modeling · Consensus signal: Simulation or modeling
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.002
Threshold uncertainty score0.006

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0010.001
Bibliometrics0.0010.000
Science and technology studies0.0000.002
Scholarly communication0.0010.002
Open science0.0010.001
Research integrity0.0010.001
Insufficient payload (model declined to judge)0.0020.000

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 head0.013
GPT teacher head0.162
Teacher spread0.149 · 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 designSimulation or modeling
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
Published2016
Admission routes1
Has abstractyes

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