Changes in the character of DOC in streams during storms in two Midwestern watersheds with contrasting land uses

• Published in: Biogeochemistry 2008-05, Vol.88 (3), p.257-270
• Main Authors: Vidon, Philippe, Wagner, Laura E, Soyeux, Emmanuel
• Format: Article
• Language: English
• Subjects: Agricultural watersheds; Agrology; Base flow; Biogeochemistry; Biogeosciences; Carbon; Creeks & streams; Dissolved organic carbon; Dissolved organic carbon character; Drains; Earth and Environmental Science; Earth Sciences; Earth, ocean, space; Ecosystems; Environmental Chemistry; Exact sciences and technology; Freshwater; Geochemistry; High flow; Hydrology; Hydrology. Hydrogeology; Land use; Life Sciences; Marine and continental quaternary; Midwest; Mineral soils; Mineralogy; Original Paper; Overland flow; Precipitation; Silicates; Soil profiles; Storm; Storms; Stormwater; Stream; Streams; Surficial geology; Tiles; Water geochemistry; Watersheds
• ISSN: 0168-2563; 1573-515X
• DOI: 10.1007/s10533-008-9207-6

Dissolved organic carbon (DOC) dynamics in streams is important, yet few studies focus on DOC dynamics in Midwestern streams during storms. In this study, stream DOC dynamics during storms in two Midwestern watersheds with contrasting land uses, the change in character of stream DOC during storms, and the usability of DOC as a hydrologic tracer in artificially drained landscapes of the Midwest are investigated. Major cation/DOC concentrations, and DOC specific UV absorbance (SUVA) and fluorescence index (FI) were monitored at 2-4 h intervals during three spring storms. Although DOC is less aromatic in the mixed land use watershed than in the agricultural watershed, land use has little impact on stream DOC concentration during storms. For both watersheds, DOC concentration follows discharge, and SUVA and FI values indicate an increase in stream DOC aromaticity and lignin content during storms. The comparison of DOC/major cation flushing dynamics indicates that DOC is mainly exported via overland flow/macropore flow. In both watersheds, the increase in DOC concentration in the streams during storms corresponds to a shift in the source of DOC from DOC originating from mineral soil layers of the soil profile at baseflow, to DOC originating from surficial soil layers richer in aromatic substances and lignin during storms. Results also suggest that DOC, SUVA and FI could be used as hydrologic tracers in artificially drained landscapes of the Midwest. These results underscore the importance of sampling streams for DOC during high flow periods in order to understand the fate of DOC in streams.