Seasonal dynamics of nitrogen in Tillamook Bay
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We characterized seasonal trends in dissolved inorganic nitrogen (N) of waters within Tillamook Bay, OR to better understand the major sources and cycling of N within the estuary. While N is an essential nutrient for ecosystem function, excess N loads into estuaries can lead to eutrophication, hypoxia, and/or decreases in biodiversity. Understanding the seasonal dynamics of N into Tillamook Bay is necessary to create focused nutrient remediation plan. Tillamook Bay is located within a developed watershed that is hydrologically influenced by both ocean tidal cycles and by discharge from five major tributaries. To understand and address the dynamics of N entering the Tillamook Bay grab samples of water at various depths were collected at 9 sites across the estuary during 8 sampling events between July 2017 and September 2018. Water samples were analyzed for concentrations of the dissolved inorganic N species nitrate (NO3-), nitrite (NO2-), and ammonium (NH4+). Nitrate was the dominant species of N found throughout the estuary with concentrations ranging from a low of 0.6 µM NO3--N in July 2017 to a high of 67.7 µM NO3--N in February 2018. Results suggest that seasonal hydrological changes can act as a strong driver of N concentrations within Tillamook Bay, with discharge from nearby rivers contributing more to total inorganic N inputs during the rainy season (October through May) and ocean tides contributing more to total inorganic N inputs during the dry season (June through September). While the seasonal changes in concentrations of different inorganic N species alone cannot provide evidence about the specific sources of N to Tillamook Bay, the results of this study provide a useful first assessment. Future studies will benefit from coupling this seasonal N data with other chemical measurements (e.g. stable isotopes of N and O), providing a more robust method for tracking the dominant source(s) of inorganic N inputs to Tillamook Bay.