Kinetics of removal of iron colloids from estuaries

Details Kinetics of removal of iron colloids from estuaries Kinetics of removal of iron colloids from estuaries

Feb 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983gecoa..47..211f&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 47, Issue 2, pp.211-216

Physics

4

Scientific paper

Laboratory experiments indicate that colloidal Fe is aggregated in estuarine waters by a second-order kinetic mechanism. The corresponding rate coefficient is proportional to the square of the salinity. A simple theoretical formulation is presented to describe the distribution of Fe in an estuary, based on observed second-order kinetics. The distribution depends on a single parameter whose value may be determined from measurements of the physical characteristics of the estuary. The theoretical expression accurately predicts observed distributions of Fe in a variety of estuaries, suggesting general applicability.

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