Estimates of benthic fluxes of nutrients across the sediment-water interface (Guarapiranga reservoir, Sao Paulo, Brazil)

Citation
Aa. Mozeto et al., Estimates of benthic fluxes of nutrients across the sediment-water interface (Guarapiranga reservoir, Sao Paulo, Brazil), SCI TOTAL E, 266(1-3), 2001, pp. 135-142
Citations number
18
Categorie Soggetti
Environment/Ecology
Journal title
SCIENCE OF THE TOTAL ENVIRONMENT
ISSN journal
00489697 → ACNP
Volume
266
Issue
1-3
Year of publication
2001
Pages
135 - 142
Database
ISI
SICI code
0048-9697(20010205)266:1-3<135:EOBFON>2.0.ZU;2-W
Abstract
Concentration profiles of nutrients (dissolved organic carbon, nitrate, nit rite, ammonium and soluble reactive phosphorus) were determined in pore wat ers from sediment from the Guarapiranga reservoir (Sao Paulo, Brazil). Redo x potential and acid volatile sulfide measurements on bulk sediment samples were determined in the field and laboratory, respectively. The sediment re dox potential ranged from - 170 to - 220 mV at 0-1 cm and increased to some what higher values at 20 cm. The acid volatile sulfide (AVS) profile had a bimodal pattern with concentration peaks at 3 cm (27-55 mg kg(-1)) and 14 c m (70-110 mg kg(-1)). Dissolved organic carbon (DOC) concentrations increas ed from the surface (4.7-5.6 mg l(-1)) to 20 cm (values up to 12 mg l(-1)). The concentration of ammonium increased significantly with depth, with max imum concentrations occurring at 15 cm; nitrate-nitrite concentrations only increased appreciably at 10 cm. The SRP profiles increased in concentratio n from the surface to approximately 10-cm depth, with a maximum value of 12 00 mug H2PO4- l(-1). Benthic fluxes from the sediment into the pore water r anged from 278 to 339 mg cm(-2) year(-1) for ammonium ions and from 8 to 18 mg cm(-2) year(-1) for SRP. These upward diffusive fluxes correspond to 47 -70% and to 10-24% of the total deposition of N and P measured in the reser voir, respectively. The burial rates for N and P in these sediments are 30- 54% and 76-89%, respectively. (C) 2001 Elsevier Science B.V. All rights res erved.