
handle: 10261/309620
La circulación estuárica en la Ría de Vigo se ve incrementada durante el verano como consecuencia del afloramiento costero. Este agua aflorada rica en NO3-, penetra por el fondo de la ría y se eleva hacia la superficie. Durante su desplazamiento hacia el exterior se forma por fotosíntesis materia orgánica particulada que sedimenta y se mineraliza a NH4+ que penetra nuevamente por el fondo junto con nueva agua rica en NO3-
1 page.-- III Reunión Ibérica sobre Fitoplancton Tóxico y Biotoxinas, Vilaxoán (Vilagarcía de Arousa, Pontevedra), 20-22 abril 1993
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