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Record W6999107513

Can alluvial landforms attenuate post-wildfire lake sedimentation rates and external phosphorus inputs?

2022· dissertation· en· W6999107513 on OpenAlexaboutno aff

Bibliographic record

VenueUWSpace (University of Waterloo) · 2022
Typedissertation
Languageen
FieldEnvironmental Science
TopicSoil and Water Nutrient Dynamics
Canadian institutionsnot available
Fundersnot available
KeywordsSedimentPhosphorusTributaryHydrology (agriculture)SedimentationParticulatesBenthic zoneSTREAMSAlluvium
DOInot available

Abstract

fetched live from OpenAlex

Severe large-scale landscape disturbance in forested source water regions by wildfire can increase the transfer of fine sediment and associated phosphorus (P) to aquatic systems. Notably, the subsequent mobilization of sediment-associated P to receiving surface waters can increase primary productivity in lakes and severely degrade water quality. The goal of this research was to examine abiotic controls on the form and mobility of particulate phosphorus (PP) in benthic sediment of an oligotrophic lake in Waterton Lakes National Park (WLNP), Alberta. In 2017, the Kenow wildfire severely burned an area of 35 000 ha which increased the transfer of pyrogenic materials to receiving streams in WLNP. The temporal distribution and concentration profiles of PP forms (non-apatite inorganic P, apatite P, organic P) and P mobility (equilibrium phosphorus concentration, EPC0) and major elements in a sediment core collected from Lower Waterton Lake (LWL) were evaluated to assess the potential of post wildfire fine sediment inputs to influence P concentrations in the overlying water column, and the potential internal loading legacy effect that wildfires may have on lake P-dynamics. Despite elevated PP levels observed in fire impacted tributaries that flow into LWL, the particulate P fractionation data show that post-fire P loading from pyrogenic materials to the lake was extremely low and only very minor post-wildfire changes in TPP speciation were observed. The presence of a large alluvial fan impeding river flow, coupled with the ingress of fine sediment in gravel bed rivers and adjacent floodplains, most likely attenuated the influx of pyrogenic materials into LWL. The mobility of PP in lake bottom sediment corresponded with historical landscape disturbances (e.g., flooding), which are likely associated with the remobilization of deposited pyrogenic materials in the alluvial fan, demonstrating a fire-flood sequence. Although the data presented in this thesis suggests that wildfire will have a minimal effect on the internal loading of P in LWL, it is increasingly acknowledged that non-stationarity due to changing climate may produce flow conditions which will resuspend and deliver pyrogenic materials to the lake, potentially creating a post-wildfire legacy effect. This thesis provides new knowledge regarding the effects of alluvial landscape forms on the post-wildfire delivery and mobility of PP into critical source water areas.

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)0.001
metaresearch head score (Gemma)0.002
Version: metacan-v3-hybrid-931329e0061cValidation 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 score0.109
Threshold uncertainty score0.217

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0010.002
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.001
Science and technology studies0.0000.001
Scholarly communication0.0010.001
Open science0.0000.000
Research integrity0.0010.000
Insufficient payload (model declined to judge)0.0030.000

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 head0.004
GPT teacher head0.187
Teacher spread0.182 · 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 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
Published2022
Admission routes1
Has abstractyes

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