Groundwater and nutrient discharge through karstic coastal springs (Castelló, Spain)

Discharge of groundwater and associated chemical compounds into coastal karstic regions, which are abundant in the Mediterranean basin, is envisaged to be significant. In this study, we evaluate the groundwater discharge and its nutrient load to the open karstic site of Badum (Castelló, East Spain)....

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Detalhes bibliográficos
Autores: Garcia-Solsona, Ester|||0000-0003-4136-9165, García Orellana, Jordi|||0000-0002-0543-2641, Masqué Barri, Pere|||0000-0002-1789-320X, Rodellas, Valentí|||0000-0002-5896-9987, Mejías, M., Ballesteros, Bruno|||0000-0002-4099-4420, Domínguez, J. A.
Tipo de documento: artigo
Data de publicação:2010
País:España
Recursos:Universitat Autònoma de Barcelona
Repositório:Dipòsit Digital de Documents de la UAB
Idioma:inglês
OAI Identifier:oai:ddd.uab.cat:130659
Acesso em linha:https://ddd.uab.cat/record/130659
https://dx.doi.org/urn:doi:10.5194/bg-7-2625-2010
Access Level:Acceso aberto
Palavra-chave:Groundwater
Springs
Karstic coastal
Biological communities
Castelló
Descrição
Resumo:Discharge of groundwater and associated chemical compounds into coastal karstic regions, which are abundant in the Mediterranean basin, is envisaged to be significant. In this study, we evaluate the groundwater discharge and its nutrient load to the open karstic site of Badum (Castelló, East Spain). Salinity profiles evidenced that groundwater discharge from coastal brackish springs causes a buoyant fresher layer, as identified with thermal infrared images. Chemical tracers (radium isotopes, dissolved inorganic silicate and seawater major elements) have been used to determine a brackish groundwater proportion in coastal waters of 36% in October 2006 and 44% in June 2007. Based on a radium-derived residence time of 2.7 days in October 2006 and 2.0 days in June 2007, total SGD fluxes have been estimated in 71 500 and 187 000m³ d⁻¹, respectively, with fresh-SGD contributions representing 71% and 85%. The calculated SGD-associated nutrient fluxes, most likely of natural origin, were 1500 and 8300 μmolm⁻² d⁻¹ of DIN and 19 and 40 μmolm⁻² d⁻¹ of DIP in October 2006 and June 2007, respectively. These inputs may actually lead to or enhance P limitation, thereby altering the structure of biological communities in the area.