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Published on: October 29, 2016
Distinct variations in fluorescent DOM components along a trophic gradient in the lower Fox River-Green Bay as
Hui Lin1, Sarah L Bartlett2, Laodong Guo3
1School of Freshwater Sciences, University of Wisconsin-Milwaukee, 600 E. Greenfield Ave., Milwaukee, WI 53204, USA; Polar Research Institute of China, 1000 Xuelong Road, Pudong, Shanghai 201209, China.
Dissolved organic matter in the Fox River-Green Bay showed a clear river source, with quality changing along the transect. Fluorescent components varied, indicating shifts in organic matter composition and lability from river to bay.
Area of Science:
- Environmental Chemistry
- Aquatic Science
- Organic Geochemistry
Background:
- Dissolved organic matter (DOM) plays a crucial role in aquatic ecosystems, influencing nutrient cycling and carbon transport.
- Understanding DOM composition and lability is essential for managing water quality in river-lake interfaces.
- The Fox River-Green Bay system is a seasonally hypereutrophic environment with dynamic water quality changes.
Purpose of the Study:
- To investigate variations in molecular weight distributions and fluorescent components of DOM along a river-to-bay transect.
- To characterize the DOM source and quality changes in the lower Fox River-Green Bay.
- To evaluate the efficacy of the one-sample PARAFAC approach for analyzing DOM.
Main Methods:
- Coupling flow field-flow fractionation (FFF) for size-separation with fluorescence excitation-emission matrix (EEM) and PARAFAC analysis.
- Utilizing a one-sample PARAFAC approach for detailed DOM characterization.
- Measuring concentrations of dissolved organic carbon and nitrogen, chromophoric DOM, and specific UV absorbance.
Main Results:
- DOM quality, indicated by decreasing DOC, DON, and specific UV absorbance, showed a strong riverine source and significant changes along the transect.
- Colloidal DOM (>1 kDa) remained a relatively constant proportion (71%) of bulk DOM, though its concentration decreased.
- Fluorescent components varied, with humic-like components (C475, C410) decreasing from river to bay, while protein-like components (C320, C290) increased.
Conclusions:
- DOM composition and quality are strongly influenced by the riverine source and undergo dynamic changes in the estuarine environment.
- The relative abundance of refractory humic-like DOM (C475) was conservative, while semi-labile humic-like DOM (C410) decreased towards the bay.
- Protein-like DOM components increased towards the bay, suggesting autochthonous production and reflecting the trophic gradient. The one-sample PARAFAC approach proved effective for DOM analysis.
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