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Record W1650105752 · doi:10.1029/2000wr000170

Two adjacent forested catchments: Dramatically different NO<sub>3</sub><sup>−</sup> export

2002· article· en· W1650105752 on OpenAlexaff
Sherry L. Schiff, K. J. Devito, Richard J. Elgood, P. M. McCrindle, John Spoelstra, Peter J. Dillon

Bibliographic record

VenueWater Resources Research · 2002
Typearticle
Languageen
FieldEnvironmental Science
TopicSoil and Water Nutrient Dynamics
Canadian institutionsUniversity of AlbertaUniversity of Waterloo
Fundersnot available
KeywordsWater tableGroundwaterSoil waterHydrology (agriculture)Drainage basinNitrateEnvironmental scienceDenitrificationNitrificationMineralization (soil science)DrainageBiogeochemical cycleGeologyNitrogenSoil scienceEnvironmental chemistryEcologyChemistry

Abstract

fetched live from OpenAlex

Two adjacent catchments with similar temperate forest cover and podzolic soils have annual nitrate (NO3−) export that differs by a factor of 10. Monthly rates of mineralization and nitrification measured by the buried bag technique, soil C/N ratios, and the contribution of microbial NO3− to total NO3− in the groundwater as determined by analysis of δ18O in NO3− are also similar. In both catchments, maximum NO3− export occurs during spring melt, but in the catchment with higher export, NO3− concentrations in the stream begin to increase in the fall period. Groundwater NO3− concentrations measured in wells are very different in the two catchments with high groundwater NO3− in the catchment exhibiting high NO3− export. Following spring melt, steeper slopes in the high NO3− catchment promote faster drainage, and the water table declines rapidly while high NO3− concentrations are maintained in groundwaters. Deeper water tables will preserve high NO3− in water infiltrating below the rooting zone and organic‐rich upper soil horizons. In the low NO3− catchment, slower drainage on shallower slopes lead to an increase in soil saturation, and the NO3− disappears from the water before the water table declines. Analyses of δ15N in NO3− during NO3− loss do not show evidence of denitrification, although denitrification proceeding to completion in isolated pockets followed by mixing with higher NO3− groundwaters would yield the same result. Alternatively, active uptake of NO3− by vegetation following spring melt will also deplete the groundwater NO3− in the shallow soil depths without isotopic fractionation. The low NO3− catchment also has lower NO3− in shallow soil waters during spring melt. Shallower slopes promote near‐surface flow paths in organic‐rich soil horizons which may facilitate denitrification during spring melt. Although the catchment with low NO3− export has a large wetland near the catchment outlet, the NO3− attenuating capacity of this wetland is largely unused except in the late fall because growing season groundwater concentrations of NO3− are undetectable and the wetland is frozen during snowmelt. In the high NO3− catchment, organic‐rich soils and vegetation in the riparian zone cannot completely attenuate high NO3− in discharging groundwaters. In our study, factors controlling NO3− in groundwater such as slope, stratigraphy, and hydraulic conductivity can play a larger role than riparian zones in controlling differences in annual NO3− export observed between catchments.

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)0.000
metaresearch head score (Gemma)0.001
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 score0.056
Threshold uncertainty score0.111

Distilled classifier scores by category (both heads)

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

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 head0.030
GPT teacher head0.267
Teacher spread0.237 · 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

Citations87
Published2002
Admission routes1
Has abstractyes

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