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Nutrient conditions in the Patraikos Gulf
Institution:1. COPPE, Federal University of Rio de Janeiro, Rio de Janeiro, Rio de Janeiro, 21941-598 Brazil;2. Computer Science Department, Federal University of Juiz de Fora, Brazil;1. DISTAV, University of Genoa, 26 Corso Europa, Genoa I-16132, Italy;2. DCCI, University of Genoa, 31 Via Dodecaneso, Genoa I-16132, Italy;3. BiGeA, University of Bologna, 1 Piazza S. Donato, Bologna I-40126, Italy;1. Departamento de Química-Física, Facultad de Ciencias del Mar y Ambientales, Universidad de Cádiz, UNESCO/UNITWIN WiCoP, Campus de Excelencia International del Mar (CEIMAR), Polígono Río San Pedro s/n, Puerto Real 11510, Cádiz, Spain;2. Centro Interdipartimentale di Ricerca per le Scienze Ambientali (C.I.R.S.A.), University of Bologna, Ravenna Campus, 48123 Ravenna, Italy;3. National Research Council-Institute of Marine Sciences (CNR-ISMAR), 40129 Bologna, Italy;4. Department of Physics and Astronomy, University of Bologna, 40127 Bologna, Italy
Abstract:The Gulf of Patras is a silled embayment opening into the Ionian Sea on the west, and through the straits of Rio into the Gulf of Corinth, on the east. The latter communicates through the Corinth canal with the Aegean Sea. Patraikos Gulf has only slightly greater concentrations of nutrients than background, in particular nitrate and silicate. A comparison is made with the nutrient concentrations in polluted coastal gulfs of the Aegean, where different nutrient levels are due to the different sources of nutrients as well as the morphology and the circulation of the waters.
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