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MEPS 233:55-71 (2002)
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Abstract
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Temporal and spatial patterns of intertidal sediment-water nutrient and oxygen fluxes in the Douro River estuary, Portugal
Catarina M. Magalhães1,*, Adriano A. Bordalo1, William J. Wiebe2
1Laboratory of Hydrobiology, Institute of Biomedical Sciences, University of Porto, 4099-003 Porto, Portugal
2Department of Marine Sciences, University of Georgia, Athens, Georgia 30602, USA
*Present address: Largo Abel Salazar 2, 4099-003 Porto, Portugal. E-mail: c_magalhaes@yahoo.com

ABSTRACT: The Douro River watershed drains 17% of the Iberian Peninsula; the present average freshwater discharge into the estuary is 488 m3 s-1. The Douro River estuary receives largely untreated sewage from about 1 million
inhabitants of Greater Porto. A major portion of the intertidal sediments is currently scheduled for removal by dredging. In order to assess their role in nutrient dynamics and productivity, sediment-water fluxes of ammonium, inorganic phosphorus,
nitrate, nitrite, silicate and oxygen were determined quarterly in muddy and sandy intertidal sediments of the lower estuary. Fluxes were estimated with both light and dark incubations. The range of net nutrient uptake rates from all sites was as follows:
ammonium 28 to 978 µmol m-2 h-1; nitrate 40 to 810 µmol m-2 h-1; nitrite 1 to 128 µmol m-2 h-1; dissolved orthophosphate 1 to 152 µmol m-2 h-1 and silicate 69 to 369
µmol m-2 h-1. Stepwise multiple regression analysis revealed strong coupling between the concentrations of most nutrients in the water column and the corresponding flux into the sediment. Mean net nutrient effluxes to the overlying
water were observed in only 6 cases out of a total of 120, and only at the muddy sediment site. Net oxygen production (light incubation) ranged from 58 to 618 mgO2 m-2 h-1, while oxygen consumption (dark incubation) ranged
from 11 to 64 mgO2 m-2 h-1. Primary production correlated significantly with chlorophyll a concentrations in the top (0.5 cm) sediment layer at the sandy sites, but showed no correlation at the muddy site. All
sampling sites were net daily sources of oxygen to the water. The net productivity of the intertidal flats and their capacity for water-column inorganic nutrient removal assumes particular importance in the Douro River estuary, a eutrophic system with a
permanently heterotrophic water column.
KEY WORDS: Douro River estuary · Intertidal flat · Sediment-water interface · Nutrient uptake · Oxygen fluxes
Full text in pdf format

Published in MEPS Vol.
233
(2002) on May 21
Print ISSN: 0171-8630; Online ISSN: 1616-1599.
Copyright © Inter-Research, Oldendorf/Luhe, 2002
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