Isotopic, trace element and nutrient characterization of coastal waters from Ubatuba inner shelf area, south-eastern Brazil


Autoria(s): POVINEC, P. P.; OLIVEIRA, J. de; BRAGA, E. S.; COMANDUCCI, J. -F.; GASTAUD, J.; GROENING, M.; LEVY-PALOMO, I.; MORGENSTERN, U.; TOP, Z.
Contribuinte(s)

UNIVERSIDADE DE SÃO PAULO

Data(s)

20/10/2012

20/10/2012

2008

Resumo

Stable 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.

Identificador

ESTUARINE COASTAL AND SHELF SCIENCE, v.76, n.3, p.522-542, 2008

0272-7714

http://producao.usp.br/handle/BDPI/32056

10.1016/j.ecss.2007.07.041

http://dx.doi.org/10.1016/j.ecss.2007.07.041

Idioma(s)

eng

Publicador

ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD

Relação

Estuarine Coastal and Shelf Science

Direitos

restrictedAccess

Copyright ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD

Palavras-Chave #submarine groundwater discharge #groundwater #seawater #river water #rain #stable isotopes #delta D #delta(IX)O #tritium #radium isotopes #radon #nutrients #trace elements #coastal zone #Ubatuba #Brazil #SUBMARINE GROUNDWATER DISCHARGE #GAMMA-RAY SPECTROMETRY #RADIUM ISOTOPES #ZONE #DONNALUCATA #MARINE #RN-222 #RA-223 #RADON #REEF #Marine & Freshwater Biology #Oceanography
Tipo

article

original article

publishedVersion