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Advisor(s)
Abstract(s)
The residence time has long been used as a classification parameter for estuaries and other semi-
enclosed water bodies. It aims to quantify the time water remains inside the estuary, being used
as an indicator both for pollution assessment and for ecological processes. Estuaries with a short
residence time will export nutrients from upstream sources more rapidly then estuaries with
longer residence time. On the other hand the residence time determines if micro-algae can stay
long enough to generate a bloom. As a consequence, estuaries with very short residence time are
expected to have much lower algae blooms, then estuaries with longer residence time. In
addition, estuaries with residence times shorter than the doubling time of algae cells will inhibit
formation of algae blooms (EPA, 2001). The residence time is also an important issue for
processes taking place in the sediment. The fluxes of particulate matter and associated adsorbed
species from the water column to the sediment depends of the particle’s vertical velocity, water
depth and residence time. This is particularly important for the fine fractions with lower sinking
velocities. The question is how to compute the residence time and how does it depend on the
computation method adopted.
Description
Keywords
Estuários 532
Citation
PECS 2002 Conference. - [S.l.], 2002. - p. 49-52
Publisher
[S.l.]