IDENTIFICATION OF NUTRIENT SOURCES IN TWO OWASCO LAKE TRIBUTARIES
We sampled eight sites along Dutch Hollow Brook and ten sites along Owasco Inlet every two weeks starting in March. Stream water was analyzed on-site for temperature, pH, conductivity, alkalinity, dissolved oxygen and stream discharge. Additional water was collected and analyzed in the lab for total phosphates, total suspended solids, silica, nitrates, and soluble reactive phosphate following standard limnological techniques. A companion study presents results from an autonomous sampler and stage recorder at Dutch Hollow Brook.
The 2011 data compared to earlier years, revealed larger flow, concentrations and fluxes, especially in Owasco Inlet. The trend parallels increased amounts of precipitation during the spring of 2011. Nutrient concentrations and fluxes (SRP, TP, TSS, and conductivity) were larger at the Benson trib. and South sites, both drain agricultural-rich land, and at Moravia and County Line sites. In contrast, concentrations and fluxes were lowest at Mill and Fillmore Creeks, which are buffered by forested land. Thus, runoff from agricultural land is a major non point source in the Owasco watershed.
The Benson tributary drains a large CAFO operation. We recommend the installation of buffer strips along this tributary, which could reduce nutrient-rich runoff. County line is probably affected by an aging waste water treatment plant, though to a lesser degree than in the past. It recently installed technologies to reduce phosphate from the effluent.
We suggest that Owasco Lake residents support mitigation and remediation within this tributary’s watershed to see if nutrient loading is reduced in the future.