dc.creatorPOVINEC, P. P.
dc.creatorOLIVEIRA, J. de
dc.creatorBRAGA, E. S.
dc.creatorCOMANDUCCI, J. -F.
dc.creatorGASTAUD, J.
dc.creatorGROENING, M.
dc.creatorLEVY-PALOMO, I.
dc.creatorMORGENSTERN, U.
dc.creatorTOP, Z.
dc.date.accessioned2012-10-20T13:44:44Z
dc.date.accessioned2018-07-04T15:52:54Z
dc.date.available2012-10-20T13:44:44Z
dc.date.available2018-07-04T15:52:54Z
dc.date.created2012-10-20T13:44:44Z
dc.date.issued2008
dc.identifierESTUARINE COASTAL AND SHELF SCIENCE, v.76, n.3, p.522-542, 2008
dc.identifier0272-7714
dc.identifierhttp://producao.usp.br/handle/BDPI/32056
dc.identifier10.1016/j.ecss.2007.07.041
dc.identifierhttp://dx.doi.org/10.1016/j.ecss.2007.07.041
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/1628690
dc.description.abstractStable isotopes, tritium, radium isotopes, radon, trace elements and nutrients data were collected during two sampling campaigns in the Ubatuba coastal area (south-eastern Brazil) with the aim of investigating submarine groundwater discharge (SGD) in the region. The isotopic composition (delta D, delta(18)O, (3)H) of submarine waters was characterised by significant variability and heavy isotope enrichment. The stable isotopes and tritium data showed good separation of groundwater and seawater groups. The contribution of groundwater in submarine waters varied from a few % to 17%. Spatial distribution of (222)Rn activity concentration in surface seawater revealed changes between 50 and 200 Bq m(-3) which were in opposite relationship with observed salinities. Time series measurements of (222)Rn activity concentration in Flamengo Bay (from 1 to 5 kBq m(-3)), obtained by in situ underwater gamma-spectrometry showed a negative correlation between the (222)Rn activity concentration and tide/salinity. This may be caused by sea level changes as tide effects induce variations of hydraulic gradients, which increase (222)Rn concentration during lower sea level, and opposite, during high tides where the (222)Rn activity concentration is smaller. The estimated SGD fluxes varied during 22-26 November between 8 and 40 cm d(-1), with an average value of 21 cm d(-1) (the unit is cm(3)/cm(2) per day). The radium isotopes and nutrient data showed scattered distributions with offshore distance and salinity. which implies that in a complex coast with many small bays and islands, the area has been influenced by local currents and groundwater-seawater mixing. SGD in the Ubatuba area is fed by coastal contaminated groundwater and re-circulated seawater (with small admixtures of groundwater). which claims for potential environmental concern with implications on the management of freshwater resources in the region. (C) 2007 Elsevier Ltd. All rights reserved.
dc.languageeng
dc.publisherACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
dc.relationEstuarine Coastal and Shelf Science
dc.rightsCopyright ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD
dc.rightsrestrictedAccess
dc.subjectsubmarine groundwater discharge
dc.subjectgroundwater
dc.subjectseawater
dc.subjectriver water
dc.subjectrain
dc.subjectstable isotopes
dc.subjectdelta D
dc.subjectdelta(IX)O
dc.subjecttritium
dc.subjectradium isotopes
dc.subjectradon
dc.subjectnutrients
dc.subjecttrace elements
dc.subjectcoastal zone
dc.subjectUbatuba
dc.subjectBrazil
dc.titleIsotopic, trace element and nutrient characterization of coastal waters from Ubatuba inner shelf area, south-eastern Brazil
dc.typeArtículos de revistas


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