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Record W7028763433

Geophysical and thermal investigations of ice-rich permafrost at Parsons Lake, Northwest Territories

2012· dissertation· en· W7028763433 on OpenAlexfundaboutno aff

Bibliographic record

VenueeScholarship@McGill (McGill) · 2012
Typedissertation
Languageen
FieldComputer Science
TopicImage Processing and 3D Reconstruction
Canadian institutionsnot available
FundersNatural Sciences and Engineering Research Council of CanadaArcticNetParks CanadaConocoPhillipsAurora Research InstituteMcGill University
KeywordsPermafrostBoreholeGround-penetrating radarDrillingInversion (geology)Disturbance (geology)SmoothingThermal
DOInot available

Abstract

fetched live from OpenAlex

Geophysical and thermal investigations of ice-rich permafrost were performed in an area of planned hydrocarbon development at Parsons Lake, Northwest Territories. The site is owned by ConocoPhillips Canada (CPC) and ExxonMobil, and is intended to be a primary target for the Mackenzie Valley Gas Project. As a result, the Program of Energy and Research Development (PERD) funded this thesis to acquire more knowledge regarding the current and future state of permafrost at this site. Information on ground temperatures and material properties are available from boreholes extracted during the 2004 CPC drilling program. In this study, the application of ground-penetrating radar (GPR) and capacitively-coupled resistivity (CCR) to map ground ice properties was tested. Since ground ice is an important factor affecting the level of disturbance initiated by thermokarst, improving the use of geophysical tools to map its nature and extent is important. By employing techniques to determine the maximum depth of investigation, optimal smoothing factors used during the inversion of raw resistivity data were computed. Once accomplished, it was found that the observed resistivity of massive ice ranged from 25 000 to 40 000 ohm-m. Conversely, values for massive ice were more widespread and overlapped with other materials like ice-rich peat when incorrect smoothing parameters were selected. The GPR cross-sections were applied to provide more detailed information on structure and contacts between massive ice and gravelly sand deposits. It was found that CCR generates similar outputs for these types of materials. One-dimensional thermal models were constructed at previously undisturbed borehole locations. Thermal outputs were compared with the observed data, and it was found that the error during the thaw season at boreholes with near-surface mineral soils is less than 1 degree celcius at any depth. When these models were used to project maximum active layer thickness changes for the period 2011-2070, subsidence is projected to begin as early as 2058. At disturbed locations, CCR surveys conducted in winter reveal two anomalies characterized by very low resistivities (< 600 ohm-m) beneath the gravel pads. One possible explanation is the development of taliks between 2004 and 2010, and thus, future fieldwork at this site is recommended. Overall, this investigation developed a model that can be used by industry to forecast near-surface thermal regime changes under varying scenarios of climate warming.

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), Science and technology studies
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 score0.585
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0010.000
Bibliometrics0.0000.001
Science and technology studies0.0010.000
Scholarly communication0.0000.002
Open science0.0010.000
Research integrity0.0010.001
Insufficient payload (model declined to judge)0.0000.000

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 head0.012
GPT teacher head0.221
Teacher spread0.209 · 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 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
Published2012
Admission routes2
Has abstractyes

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