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Record W3091436045

LABORATORY SCALE EVALUATION OF THE FEASIBILITY OF USING GUANIDINIUM SALTS AS A MEANS OF INSITU SOIL STRENGTHENING FOR WEAK CLAYS

2020· dissertation· en· W3091436045 on OpenAlexaboutno aff
Adam Benjamin Leik

Bibliographic record

VenueUniversity Library (University of Saskatchewan) · 2020
Typedissertation
Languageen
FieldEnvironmental Science
TopicLandfill Environmental Impact Studies
Canadian institutionsnot available
Fundersnot available
KeywordsScale (ratio)Environmental chemistryEnvironmental scienceChemistryGeographyCartography
DOInot available

Abstract

fetched live from OpenAlex

Deep-seated, slow moving landslides are widespread throughout the prairie provinces of Canada, especially in Saskatchewan and eastern Alberta. These landslides are characterized by a thick deposit of glacial drift underlain by poorly lithified cretaceous shale (Bearpaw, Lea Park formations). Multiple thin layers of extremely weak, smectite rich, clayey soils are often found within the upper portions of these cretaceous shale formations. The interfaces of these smectitic clay lenses typically produce a pronounced shear plane, turning the overlying soils into a large slump block. Landslides of this nature can span several hundred meters in length, which provides a threat to infrastructure such as roads, bridges, and pipelines.\n\nDue to the depth of these shear zones, and the scale of these types of creeping failures, remediation via traditional geotechnical engineering solutions is either not feasible or extremely costly to pursue. The lack of available solutions for this common problem has prompted research that stems from a multi-disciplinary approach. The current research is intended to evaluate the feasibility of modifying the porewater chemistry of these smectitic shear zones by using guanidinium chloride to propagate mineralogical alteration through ion exchange, as a means of insitu soil strengthening.\n\nThis study was limited to laboratory scale testing. The specific objectives for this research were to: i.) characterise the mechanism by which guanidinium salts can alter the mineralogical and macroscopically observable properties of natural expansive clay soils; and, ii.) assess fundamental questions pertaining to the full-scale implementation of the proposed insitu strengthening technique.\n\nA local prairie soil, Regina Clay, was used for the majority of testing procedures, as it is readily available and is representative of the types of soils associated with the problem that this research aimed to address. The results from a series of batch-style geotechnical and mineralogical testing procedures contributed to a clearer understanding of the mechanisms associated with this treatment, the required strengths of saline solution for treatment, quantified the effects of treatment, and the permanence of the effects associated with this treatment.\n\nTreating expansive soils with concentrations of 0.1 molar guanidinium chloride saline solutions were found to cause permanent alterations to the smectite mineral’s basal spacing and soil fabric, increase the permeability by half an order of magnitude, and increase the residual shear strength by up to 100%, all without reducing the oedometric stiffness.\nAs the present study is limited to laboratory-scale trials, a full-scale test site is recommended to further validate the effects found in this research. However, despite the limitations of this work, the potential for insitu soil strengthening via guanidinium salts appears to be significant.

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 distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Qualitative · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.317
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0000.001
Science and technology studies0.0000.001
Scholarly communication0.0000.001
Open science0.0010.001
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 head0.022
GPT teacher head0.223
Teacher spread0.201 · 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 teacher head, not a consensus.

Study designQualitative
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
Published2020
Admission routes1
Has abstractyes

Explore more

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