Fresh meteoric versus recirculated saline groundwater nutrient inputs into a subtropical estuary

Mahmood Sadat-Noori; Isaac R Santos; Douglas R Tait; Damien T Maher

doi:10.1016/j.scitotenv.2016.06.008

Fresh meteoric versus recirculated saline groundwater nutrient inputs into a subtropical estuary

Sci Total Environ. 2016 Oct 1:566-567:1440-1453. doi: 10.1016/j.scitotenv.2016.06.008. Epub 2016 Jun 17.

Authors

Mahmood Sadat-Noori¹, Isaac R Santos², Douglas R Tait³, Damien T Maher⁴

Affiliations

¹ National Marine Science Centre, School of Environment, Science and Engineering, Southern Cross University, Coffs Harbour, NSW, Australia; School of Environment, Science and Engineering, Southern Cross University, Lismore, NSW, Australia. Electronic address: mahmood.sadat-noori@scu.edu.au.
² National Marine Science Centre, School of Environment, Science and Engineering, Southern Cross University, Coffs Harbour, NSW, Australia.
³ National Marine Science Centre, School of Environment, Science and Engineering, Southern Cross University, Coffs Harbour, NSW, Australia; School of Environment, Science and Engineering, Southern Cross University, Lismore, NSW, Australia.
⁴ School of Environment, Science and Engineering, Southern Cross University, Lismore, NSW, Australia.

PMID: 27320738
DOI: 10.1016/j.scitotenv.2016.06.008

Abstract

The role of groundwater in transporting nutrients to coastal aquatic systems has recently received considerable attention. However, the relative importance of fresh versus saline groundwater-derived nutrient inputs to estuaries and how these groundwater pathways may alter surface water N:P ratios remains poorly constrained. We performed detailed time series measurements of nutrients in a tidal estuary (Hat Head, NSW, Australia) and used radium to quantify the contribution of fresh and saline groundwater to total surface water estuarine exports under contrasting hydrological conditions (wet and dry season). Tidally integrated nutrient fluxes showed that the estuary was a source of nutrients to the coastal waters. Dissolved inorganic nitrogen (DIN) export was 7-fold higher than the average global areal flux rate for rivers likely due to the small catchment size, surrounding wetlands and high groundwater inputs. Fresh groundwater discharge was dominant in the wet season accounting for up to 45% of total dissolved nitrogen (TDN) and 48% of total dissolved phosphorus (TDP) estuarine exports. In the dry season, fresh and saline groundwater accounted for 21 and 33% of TDN export, respectively. The combined fresh and saline groundwater fluxes of NO3, PO4, NH4, DON, DOP, TDN and TDP were estimated to account for 66, 58, 55, 31, 21, 53 and 47% of surface water exports, respectively. Groundwater-derived nitrogen inputs to the estuary were responsible for a change in the surface water N:P ratio from typical N-limiting conditions to P-limiting as predicted by previous studies. This shows the importance of both fresh and saline groundwater as a source of nutrients for coastal productivity and nutrient budgets of coastal waters.

Keywords: Groundwater–surface water interaction; Phosphorus; Radium isotopes; Submarine groundwater discharge; Subterranean estuary.