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Record W1913085309 · doi:10.11575/prism/27281

Peatland Biogeochemistry and Plant Productivity Responses to Field-based Hydrological and Temperature Simulations of Climate Change

2014· dissertation· en· W1913085309 on OpenAlexaboutno aff
Tariq Muhammad Munir

Bibliographic record

VenuePRISM (University of Calgary) · 2014
Typedissertation
Languageen
FieldEnvironmental Science
TopicPeatlands and Wetlands Ecology
Canadian institutionsnot available
Fundersnot available
KeywordsBiogeochemistryClimate changeProductivityEnvironmental scienceField (mathematics)ClimatologyPeatHydrology (agriculture)Atmospheric sciencesGeologyEcologyOceanographyEconomicsBiology

Abstract

fetched live from OpenAlex

Northern peatlands have accumulated approximately one third of all soil carbon (C) and therefore play an important role in the global C cycle. Besides the C sink function, peatlands are one of the largest biological sources of atmospheric methane (CH4) and represent approximately 10% of global soil nitrogen (N) stocks. These ecosystems are present at latitudes that are predicted to be highly sensitive to climate change that will likely result in deeper water table positions. The reduction in soil moisture may increase peat decomposition rates and consequently affect nutrient dynamics. While attempts have been made to assess the impact of climate change on peatland C gas exchange and nutrient dynamics, controlled field experimentation remains limited. Therefore, the objectives of this thesis were to estimate the responses of peatland carbon dioxide (CO2) and CH4 flux, nutrient dynamics, and plant productivity to a recent- and a ten-year old drainage, and a warming treatment induced by open-top chambers, across the peatland’s hummock-hollow microtopography. The study was carried out at a dry continental treed bog in boreal Alberta during 2011-2013. Water level drawdown in the longer-term resulted in shifts in biomass coverage and plant community composition between the microforms. The moss biomass was replaced by vascular plant biomass (mostly woody shrubs) at hummocks, and by lichen biomass at hollows. The shift in dominant vegetation was reflected in CO2 fluxes; the longer-term drained hummocks were the largest sink of CO2 while hollows at the same site were the largest sources. While the short- and longer-term drained sites were net sources of CO2, the warming treatment converted the longer-term drained site to a sink of CO2-C. Water table drawdown greatly reduced CH4 flux at both hummocks and hollows, and the reduction increased with time. The warming treatment increased emissions of CH4 at hollows and increased consumption of CH4 at hummocks. The extractable and available nutrient pools in the peat soil increased with deepening of water level, and over time. The water level driven dynamics of peat nutrient pools were reflected in the vegetation C:N ratio. The warming treatment increased nutrient pools more at hummocks than at hollows and the impact increased with time. Based on these results, I suggest that, models of peatland development need to include C and nutrient cycling links to moisture and temperature parameters to better predict plant productivity and C exchange under changing climatic conditions.

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 score0.086
Threshold uncertainty score0.502

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 integrity0.0000.000
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 head0.008
GPT teacher head0.203
Teacher spread0.195 · 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

Citations3
Published2014
Admission routes1
Has abstractyes

Explore more

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