Nitrogen transformations along a shallow subterranean estuary

• Main Authors: M. Couturier, G. Tommi-Morin, M. Sirois, A. Rao, C. Nozais, G. Chaillou
• Format: Article
• Language: English
• Published: Copernicus Publications 2017-07-01
• Series: Biogeosciences
• Online Access: https://www.biogeosciences.net/14/3321/2017/bg-14-3321-2017.pdf
• ISSN: 1726-4170; 1726-4189

The transformations of chemical constituents in subterranean estuaries (STEs) control the delivery of nutrient loads from coastal aquifers to the ocean. It is important to determine the processes and sources that alter nutrient concentrations at a local scale in order to estimate accurate regional and global nutrient fluxes via submarine groundwater discharge (SGD), particularly in boreal environments, where data are still very scarce. Here, the biogeochemical transformations of nitrogen (N) species were examined within the STE of a boreal microtidal sandy beach located in the Magdalen Islands (Quebec, Canada). This study revealed the vertical and horizontal distribution of nitrate (NO₃⁻), nitrite (NO₂⁻), ammonia (NH₄⁺), dissolved organic nitrogen (DON) and total dissolved nitrogen (TDN) measured in beach groundwater during four spring seasons (June 2011, 2012, 2013 and 2015) when aquifer recharge was maximal after snowmelt. Inland groundwater supplied high concentrations of NO_<i>x</i> and DON to the STE, whereas inputs from seawater infiltration were very limited. Non-conservative behaviour was observed along the groundwater flow path, leading to low NO_<i>x</i> and high NH₄⁺ concentrations in the discharge zone. The long transit time of groundwater within the beach (∼ 166 days), coupled with oxygen-depleted conditions and high carbon concentrations, created a favourable environment for N transformations such as heterotrophic and autotrophic denitrification and ammonium production. Biogeochemical pathways led to a shift in nitrogen species along the flow path from NO_<i>x</i>-rich to NO_<i>x</i>-poor groundwater. An estimate of SGD fluxes of N was determined to account for biogeochemical transformations within the STE based on a N-species inventory and Darcy's flow. Fresh inland groundwater delivered 37 mol NO_<i>x</i> yr⁻¹ per metre of shoreline and 63 mol DON m⁻¹ yr⁻¹ to the STE, and NH₄⁺ input was negligible. Near the discharge zone, the potential export of N species was estimated around 140, 1.5 and 33 mol yr⁻¹ per metre of shoreline for NH₄⁺, NO_<i>x</i> and DON respectively. In contrast to the fresh inland groundwater, the N load of beach groundwater near the discharge zone was dominated by NH₄⁺ and DON. Our study shows the importance of tidal sands in the biogeochemical transformation of the terrestrial N pool. This local export of bioavailable N probably supports benthic production and higher trophic levels leading to its rapid transformation in surface sediments and coastal waters.