MétaCan
Menu
Back to cohort
Record W7029348703

Integrating thermal, geological and hydrogeologic methods to study fractured carbonate rock hydrogeology

2016· dissertation· en· W7029348703 on OpenAlexaboutno aff

Bibliographic record

VenueeScholarship@McGill (McGill) · 2016
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicKarst Systems and Hydrogeology
Canadian institutionsnot available
Fundersnot available
KeywordsHydrogeologyCarbonateCarbonate rockWork (physics)
DOInot available

Abstract

fetched live from OpenAlex

Proper management of carbonate rock aquifers requires an understanding of the aquifers hydraulic properties and flow dynamics. Faulted carbonate rock aquifers have complex permeability patterns, as faults can act as hydraulic conduits, barriers or combined conduit-barrier systems. Integrated, multi-disciplinary methods are needed in order to gain a more comprehensive understanding of fractured carbonate rock hydrogeology. The objective of this thesis is to use thermal, geological and hydrogeologic methods to better understand fractured rock hydrogeology of carbonate rocks. This was completed using two study areas: 1) an unused quarry in St. Dominique, Quebec, Canada, and 2) an outcrop of the Champlain Thrust fault at Lone Rock Point, Burlington, Vermont, USA. Thermal imagery of groundwater seeps at the quarry was collected over a 22-month period to determine the efficacy of using thermal imagery to quantify groundwater discharge. Thermal imagery is effective at locating and qualitatively characterizing the flux of groundwater seeps. However, the application of thermal imagery is limited by diverse factors including technical issues of image acquisition, diurnal changes in radiation and temperature, and rock face heterogeneity. Groundwater discharge rates could not be directly quantified from thermal imagery in either winter or summer because of these limitations. At the outcrop of the Champlain Thrust fault, structural geology observations were integrated with surficial and subsurface hydrogeological observations. Here, the fault core thickness thickens on the meter-scale, splays out into multiple strands and is offset by a minor normal fault. Groundwater seeps are prevalent in the heavily fractured footwall but limited in the fault core and hanging wall, suggesting at the cliff face the water table is generally near the fault core and groundwater flow in the hanging wall is limited. At the well field, the Champlain Thrust fault is offset significantly by a high-angle structure, the water table is near the surface and aquifer pumping tests reveal a complex hydrogeologic system, with karst and steep fractures as strong hydraulic conduits in the hanging wall and fault core. The most salient features of the fault zone hydrogeology in the surface and subsurface data are different but can be integrated into a preliminary conceptual model. Together the surface and subsurface methods underscore and emphasize the complexity and heterogeneity of the hydrogeology of this low angle sedimentary fault.

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)0.003
metaresearch head score (Gemma)0.001
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesMeta-epidemiology (narrow), Science and technology studies, Research integrity, Insufficient payload (model declined to judge)
Consensus categoriesMeta-epidemiology (narrow), Insufficient payload (model declined to judge)
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: none
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.778
Threshold uncertainty score1.000

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0030.001
Meta-epidemiology (narrow)0.0010.001
Meta-epidemiology (broad)0.0020.000
Bibliometrics0.0010.001
Science and technology studies0.0020.000
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0020.002
Insufficient payload (model declined to judge)0.0040.001

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 head0.018
GPT teacher head0.272
Teacher spread0.254 · 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; both teacher heads agree on what is shown here.

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
Published2016
Admission routes1
Has abstractyes

Explore more

Same venueeScholarship@McGill (McGill)Same topicKarst Systems and HydrogeologyFrench-language works237,207