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Record W2012830191 · doi:10.1021/es0000753

Temporal Trends in the Isotope Signature of Air-Borne Sulfur in Central Europe

2000· article· en· W2012830191 on OpenAlexaboutno aff
Martin Novák, Iva Jačková, Eva Přechová

Bibliographic record

VenueEnvironmental Science & Technology · 2000
Typearticle
Languageen
FieldEarth and Planetary Sciences
TopicGroundwater and Isotope Geochemistry
Canadian institutionsnot available
Fundersnot available
KeywordsSeasonalityδ34SSulfateNorthern HemisphereEnvironmental scienceAtmosphere (unit)Isotopic signatureAtmospheric sciencesAir pollutionPollutionScavengingSulfurSulfur dioxideEnvironmental chemistrySulfate aerosolAir mass (solar energy)IsotopeChemistryMeteorologyGeologyGeographyEcology

Abstract

fetched live from OpenAlex

In various parts of the Northern hemisphere air-borne S exhibits a seasonality, with isotopically light (i.e., 32S-rich) sulfur predominating in the warm summer months. Such seasonality has been reported from the United States, Canada, Japan, and China. Elevated biological emissions of isotopically light S in summer, a temperature-dependent isotope fractionation accompanying the oxidation of SO2, and heavy rains in winter bringing 34S-rich marine S have been suggested as the controlling mechanisms. In the atmosphere of Central Europe, one of the most severely polluted regions of the world, we have found an opposite seasonal trend: Isotopically light SO2-S predominates in the cold winter months, whereas isotopically heavy SO2-S is typical of the summer. The low delta34S values of air-borne SO2 in winter are influenced by low-delta34S emissions from local coal-burning power plants. The coal contains isotopically light S (mean delta34S of 1.6/1000). Higher demand for electricity during the heating season leads to higher anthropogenic S emission rates in winter. On a yearly basis, atmospheric sulfate S in Central Europe is isotopically heavier than atmospheric SO2-S by 4/1000. Atmospheric oxidation of SO2 is accompanied by an isotope fractionation resulting in 34S-enriched sulfate. In addition to the seasonality in air-borne delta34S(SO2), we report also an interannual trend of 1/1000 yr(-1) toward isotopically light sulfate S in atmospheric deposition. This interannual trend cannot be explained by a change in pollution sources accompanying the present massive environmental cleanup. To investigate the role of biological S emissions from the soil of heavily polluted ecosystems, we conducted a series of laboratory experiments using repacked soil columns and 34S-enriched precipitation under summer and winter temperatures. These experiments indicate that, under summer temperatures, the 34S-labeled precipitation is largely captured by the upper organic-rich soil horizons, a high proportion (53-74%) of S input is revolatilized, and the biologically reemitted S is isotopically light. Under winter temperatures more precipitation S is leached to the bottom of the soil columns. Our experiments have shown that biological emissions in Central Europe can be sizable. Yet, they cannot be singled out in the overall SO2 isotope pattern in the atmosphere. The main reason is continuous, variable (0-4/1000), open-system depletion in 34S in the residual SO2 during the isotopically selective SO2-to-SO4(2-) conversion.

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 categoriesInsufficient payload (model declined to judge)
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.083
Threshold uncertainty score0.997

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.002
Science and technology studies0.0000.001
Scholarly communication0.0000.000
Open science0.0010.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0040.000

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 head0.180
Teacher spread0.176 · 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.

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

Citations81
Published2000
Admission routes1
Has abstractyes

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