Abstract
Sediment and nutrient exports were evaluated in a small agriculture-dominated watershed that drains into Rondeau Bay, on the northern shore of Lake Erie in Southwestern Ontario, Canada. The following hypothesis was tested: the quantity and quality of suspended sediment yields in agricultural settings controls nutrient transfer from surface runoff. Stream discharge and water quality were monitored at three locations along a tributary reach within the Rondeau Bay basin during the 2013 growing-harvest season (May–October). Water samples were analyzed in the laboratory for suspended sediment concentration, particle size, and sediment-assisted nitrogen and phosphorus content. Estimated total sediment yield over the 6-month monitoring period was ∼50t (0.13tha−1). A mid-season change in contributing sediment sources was inferred based on the observations of suspended sediment transfer and particle size following a ∼92mm rainfall event. This extreme runoff event marked a change in the discharge-suspended sediment response seen in the catchment, which included a July–September abrupt decrease in suspended sediment concentration and a coincident increase in fine-grained particle abundance. Clockwise event hysteresis suggested adjacent and/or likely channel derived sediment sources. Finally, there was a positive relationship between suspended sediment concentration and phosphorus (R2=0.86, n=63) and orthophosphate (R2=0.75, n=63). Estimated nutrient concentrations exceeded provincial load guidelines, which suggests that present land management efforts to minimize nutrient loading via surface runoff require further evaluation. This research concludes that agricultural-based nutrient loading into Lake Erie is sediment-assisted and that this sediment potentially derives from in-channel and tile drain sources. The findings have important implications for future soil loss and thus nutrient loading from agricultural settings, especially during extreme events.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.