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Record W7047835600

Holocene paleohydrological variability and change in the Timmins region, Ontario, Canada

2019· dissertation· en· W7047835600 on OpenAlexaboutno aff

Bibliographic record

VenueQSpace (Queen's University Library) · 2019
Typedissertation
Languageen
FieldPhysics and Astronomy
TopicSuperconducting and THz Device Technology
Canadian institutionsnot available
Fundersnot available
KeywordsHoloceneClimate changeGroundwaterWater balancePeriod (music)PollenHydrology (agriculture)Elevation (ballistics)Sea level
DOInot available

Abstract

fetched live from OpenAlex

Climate models suggest that temperatures will increase by at least 1.5-2°C by the end of the 21st century due to climate change. Similar patterns were observed during the mid-Holocene when the American prairie region displayed drier conditions while the American northeast was wetter. Published pollen records in northeast Ontario give conflicting perspectives and, it remains poorly understood whether this area was drier or wetter during this period. The overall objective of this dissertation is to better understand paleohydrological variability and change over the Holocene in the Timmins region of Ontario and to investigate the role of groundwater connectivity in how lakes respond to hydroclimatic changes. 
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\nBased on lake-water geochemistry, Chapter 2 shows that elevation is the main control on lake-water-groundwater interactions at the landscape level and that the water balance in lakes varied between field campaigns with upland lakes showing a greater sensitivity to short-term and seasonal hydroclimatic change as well as to evaporative drawdown. 
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\nIn order to understand how water levels varied over a long-term perspective, sediment cores were retrieved from two adjacent lakes: one located upland and limited to the local groundwater system (Irrigation Lake); and the other positioned at a lower elevation and embedded in a regional aquifer (Charland Lake). Chapters 3 and 4 aim at reconstructing past hydrological conditions using pollen along with carbonate stable isotopes, and sediment elemental chemistry respectively. Both chapters concluded that water levels were lower between 9,500 and 6,500 years Before Present (BP) after which they rose rapidly between 6,500 and 5,200 years BP to reach stable water highstands between 5,200 and 1,600 years BP, after which levels decreased slightly while remaining relatively high from 1,600 years BP to present. This implies that northeast Ontario is synchronous with the American northeast and asynchronous with the American prairie region. However, those changes were less pronounced in Charland Lake, indicating that buffering from groundwater dampens even sustained long-term hydroclimatic change, in comparison to the higher elevation record from Irrigation Lake. This suggests that lakes will respond differentially to future climate change based on their degree of connectedness to the groundwater system.

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 categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.339
Threshold uncertainty score0.950

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.001
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 head0.010
GPT teacher head0.187
Teacher spread0.177 · 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.

The models applied no category: nothing in the taxonomy fit this work.
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
Published2019
Admission routes1
Has abstractyes

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