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Evaluation of ammonium and phosphate release from intertidal and subtidal sediments of a shallow coastal lagoon (Ria Formosa – Portugal): a modelling approach

dc.contributor.authorSerpa, Dalila
dc.contributor.authorFalcão, Manuelapor
dc.contributor.authorDuarte, Pedro
dc.contributor.authorCancela da Fonseca, Luís
dc.contributor.authorVale, Carlospor
dc.date.accessioned2007-07-31T14:53:52Zpor
dc.date.accessioned2011-10-06T14:40:32Z
dc.date.available2007-07-31T14:53:52Zpor
dc.date.available2011-10-06T14:40:32Z
dc.date.issued2007por
dc.description.abstractDuring an annual cycle, overlying water and sediment cores were collected simultaneously at three sites (Tavira, Culatra and Ramalhete) of Ria Formosa’s intertidal muddy and subtidal sandy sediments to determine ammonium, nitrates plus nitrites and phosphate. Organic carbon, nitrogen and phosphorus were also determined in superficial sediments. Ammonium and phosphate dissolved in porewater were positively correlated with temperature (P < 0.01) in muddy and sandy sediments, while the nitrogen-oxidized forms had a negative correlation (P < 0.02) in muddy sediments probably because mineralization and nitrification/denitrification processes vary seasonally. Porewater ammonium profiles evidenced apeak in the top-most muddy sediment (380 lM) suggesting higher mineralization rate when oxygen is more available, while maximum phosphate concentration (113 lM) occurred in the sub-oxic layer probably due to phosphorus desorption under reduced conditions. In organically poor subtidal sandy sediments, nutrient porewater concentrations were always lower than in intertidal muddy sediments, ranging annually from 20 lMto 100 lM for ammonium and from 0.05 lM to 16 lM for phosphate. Nutrient diffusive fluxes predicted by a mathematical model were higher during summer, inbothmuddy (104 nmol cm–2d–1––NH4+; 8 nmol cm–2 d–1––HPO4–2) and sandy sediments (26 nmol cm–2 d–1––NH4+; 1 nmol cm–2 d–1––HPO4–2), while during lower temperature periods these fluxes were 3–4 times lower. Based on simulated nutrient effluxes, the estimated annual amount of ammonium and phosphate exported from intertidal areas was three times higher than that released from subtidal areas (22 ton year–1––NH4+; 2 ton year–1––HPO4–2), emphasizing the importance of tidal flats to maintain the high productivity of the lagoon. Global warming scenarios simulated with the model, revealed that an increase in lagoon water temperature only produces significant variations (P < 0.05) for NH4+ in porewater and consequent diffusive fluxes, what will probably affect the system productivity due to a N/P ratio unbalance.por
dc.identifier.citationBiogeochemistry (82) (2007), pp. 291–304por
dc.identifier.urihttp://hdl.handle.net/10284/275por
dc.language.isoengpor
dc.publisherSpringerpor
dc.relation.ispartofseriesBiogeochemistrypor
dc.relation.ispartofseries82, 2007por
dc.subjectAmmoniumpor
dc.subjectCoastal lagoonpor
dc.subjectGeochemical processespor
dc.subjectModellingpor
dc.subjectPhosphate Ria Formosapor
dc.titleEvaluation of ammonium and phosphate release from intertidal and subtidal sediments of a shallow coastal lagoon (Ria Formosa – Portugal): a modelling approachpor
dc.typejournal article
dspace.entity.typePublication
person.familyNameSerpa
person.familyNameDuarte
person.familyNameCancela da Fonseca
person.givenNameDalila
person.givenNamePedro
person.givenNameLuís
person.identifier158912
person.identifier.ciencia-id221A-65A5-3D4F
person.identifier.ciencia-idF614-0053-05A5
person.identifier.ciencia-idC01F-F68E-2327
person.identifier.orcid0000-0001-7808-963X
person.identifier.orcid0000-0001-7461-605X
person.identifier.orcid0000-0001-6527-0827
person.identifier.ridF-5250-2012
person.identifier.ridF-1247-2014
person.identifier.ridI-5564-2012
person.identifier.scopus-author-id23490709400
person.identifier.scopus-author-id7005201821
person.identifier.scopus-author-id8640178100
rcaap.rightsopenAccesspor
rcaap.typearticlepor
relation.isAuthorOfPublication7963d777-41f3-4198-b12a-29e2e4cb573c
relation.isAuthorOfPublicationde486bab-75c6-4f98-8ee1-b27b20edbe2d
relation.isAuthorOfPublicatione3de5d29-71b0-499d-ada4-61434413fc7a
relation.isAuthorOfPublication.latestForDiscoveryde486bab-75c6-4f98-8ee1-b27b20edbe2d

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