Sediments can play an important role in estuarine ecosystems by buffering e
nvironmental nutrient concentrations in overlying waters. This study examin
ed the role of surface chemistry in controlling the release of NH4+ from re
suspended sediments in the large, shallow, negative estuary Laguna Madre, T
X. Two techniques were used: a generally accepted elutriate method in which
sediments were added at a 1:5 ratio to overlying water and a more dilute p
rocedure (closed) where sediments were added at three ratios ranging from 1
:10,000 to 1:100. In general, the more dilute procedure resulted in greater
release of NH4+ from sediments. This is the result of the relative positio
ns that the final solution concentrations place the systems on for an exper
imentally determined Langmuir-type adsorption isotherm. The closed system t
echnique also indicated that approximately equal amounts of the released NH
4+ came from porewater, loosely-bound quick-release, and tightly-bound slow
-release fractions. Experimental results were supported by observations dur
ing dredging activities. Model calculations indicate that resuspension even
ts may cause NH4+ releases comparable to NH4+ fluxes from bottom sediments.
Resuspension could potentially contribute to such environmental problems i
n this estuary as the 'brown tide'. (C) 1999 Published by Elsevier Science
B.V.