Spatial Influences on Rates of Denitrification in Floridan Karst Aquifers

Nitrogen is a major contaminant of waterways throughout the world. This nitrogen is derived from a variety of sources including fertilizers, municipal wastewater, and atmospheric deposition. There has been a historical focus on nitrogen loading in surface waters, but in recent times this focus has shifted to denitrification. Denitrification is a major processes in which nitrogen is removed from waterways especially aquifers, which are often low in dissolved oxygen a critical factor for denitrification. This study focuses on the spatial relationships that influence this process using dissolved oxygen, nitrogen, and δ15N-NO3- data collected from a previous study in the karst Floridan Aquifer System by Heffernan et al. (2012). This data is compared to and various spatial datasets in order to understand their influence on these parameters. Many previous research studies have already shown how land covers exports varying amounts of nitrogen. Changes in nitrogen export between various landuses will change the amount of nitrogen entering a waterway. This study identified a relationship between landuse and different rates of dissolved oxygen, nitrogen loading, and denitrification. This paper also identified a strong relationship between wastewater treatment plant discharge that is land applied to changes in nitrogen loading and denitrification. To add further credence to the relationships between landuse and nitrogen a comparison of the isotope data collected in the Heffernan et al. (2012) was conducted. This comparison identified particular that various landuses show trends regarding their isotopic composition.