Molecular Weight Distributions and Size-dependent Composition of Dissolved Organic Matter in the Aquatic Continuum
Why this work is in the frame
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Bibliographic record
Abstract
Dissolved organic matter (DOM) in aquatic environments is one of the most important carbon reservoirs in global carbon cycling. The molecular weight of DOM is strongly related to a great number of biogeochemical reactions, influencing ecological functions and the fate of bioactive elements in aquatic ecosystems. A new technique coupling flow field-flow fractionation with fluorescence excitation-emission matrix (EEM) and parallel factor (PARAFAC) analysis was developed to elucidate the variations in DOM composition and optical properties with molecular weight in the individual samples and their changes along the aquatic continuum. Based on the novel coupling technique, variations in DOM characteristics were investigated across a trophic gradient from the lower Fox River to open Green Bay. Humic-like components were predominantly partitioned in the lower molecular weight fractions while protein-like components were mostly in the higher molecular weight fractions. Furthermore, unique fluorescent components in the river and open bay waters were observed, which would not have been identified using classic EEM-PARAFAC approach. Three fluorescent DOM components, including two humic-like and one protein-like components, were first reported for the lower Yukon River. Together with seasonal changes in chemical composition and optical properties between different DOM size-fractions, we provide a baseline dataset for future trend studies in the context of environmental change in Arctic river basins. A data fusion technique was applied to jointly analyze multiple datasets including fluorescence EEM and Fourier transform infrared spectra to decipher potential internal connections between fluorophores and chemical bonds. Humic-like components were mostly associated with C-H, C=C, and C-O bonds, while protein-like components were correlated more with C-N and N-H bonds. Based on year-long time-series sampling, seasonal variations of DOM size and composition were further investigated in two contrasting aquatic environments, i.e., the terrestrial-dominated Milwaukee River, with environmental changes and anthropogenic impacts from metropolitan Milwaukee, and the eutrophic Veterans Park Lagoon, where seasonal Microcystis blooms have been observed over the past decades. In addition to differences in DOM sources and composition, which were correlated to hydrological conditions and biomass, factors controlling DOM dynamics and seasonality were distinctive between the two aquatic ecosystems.
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Full frame distilled prediction
Teacher imitationNot 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.
Codex and Gemma teacher scores by category
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.000 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.000 | 0.000 |
| Science and technology studies | 0.000 | 0.000 |
| Scholarly communication | 0.000 | 0.000 |
| Open science | 0.000 | 0.000 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.000 | 0.000 |
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.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it