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1000 Titel
  • Storm-Driven Fresh Submarine Groundwater Discharge and Nutrient Fluxes From a Barrier Island
1000 Autor/in
  1. Adyasari, Dini |
  2. Montiel, Daniel |
  3. Mortazavi, Behzad |
  4. Dimova, Natasha |
1000 Erscheinungsjahr 2021
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2021-07-27
1000 Erschienen in
1000 Quellenangabe
  • 8
1000 Copyrightjahr
  • 2021
1000 Embargo
  • 2022-01-29
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.3389/fmars.2021.679010 |
1000 Publikationsstatus
1000 Abstract/Summary
  • <jats:p>Quantifying and characterizing groundwater flow and discharge from barrier islands to coastal waters is crucial for assessing freshwater resources and contaminant transport to the ocean. In this study, we examined the groundwater hydrological response, discharge, and associated nutrient fluxes in Dauphin Island, a barrier island located in the northeastern Gulf of Mexico. We employed radon (<jats:sup>222</jats:sup>Rn) and radium (Ra) isotopes as tracers to evaluate the temporal and spatial variability of fresh and recirculated submarine groundwater discharge (SGD) in the nearshore waters. The results from a 40-day continuous <jats:sup>222</jats:sup>Rn time series conducted during a rainy season suggest that the coastal area surrounding Dauphin Island was river-dominated in the days after storm events. Groundwater response was detected about 1 week after the precipitation and peak river discharge. During the period when SGD was a factor in the nutrient budget of the coastal area, the total SGD rates were as high as 1.36 m day<jats:sup>–1</jats:sup>, or almost three times higher than detected fluxes during the river-dominated period. We found from a three-endmember Ra mixing model that most of the SGD from the barrier island was composed of fresh groundwater. SGD was driven by marine and terrestrial forces, and focused on the southeastern part of the island. We observed spatial variability of nutrients in the subterranean estuary across this part of the island. Reduced nitrogen (i.e., NH<jats:sub>4</jats:sub><jats:sup>+</jats:sup> and dissolved organic nitrogen) fluxes dominated the eastern shore with average rates of 4.88 and 5.20 mmol m<jats:sup>–2</jats:sup> day<jats:sup>–1</jats:sup>, respectively. In contrast, NO<jats:sub>3</jats:sub><jats:sup>–</jats:sup> was prevalent along the south-central shore, which has significant tourism developments. The contrasting nutrient dynamics resulted in N- and P-limited coastal water in the different parts of the island. This study emphasizes the importance of understanding groundwater flow and dynamics in barrier islands, particularly those urbanized, prone to storm events, or located near large estuaries.</jats:p>
1000 Sacherschließung
lokal storm
lokal radon
lokal hydrological response
lokal northern Gulf of Mexico
lokal radium
lokal nutrient
lokal barrier island
lokal submarine groundwater discharge
lokal Marine Science
1000 Liste der Beteiligten
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1000 Erstellt am 2024-04-11T07:05:07.127+0200
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1000 Zuletzt bearbeitet Tue May 07 12:54:39 CEST 2024
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