G. Williams et al., THE BEHAVIOR OF NATURAL AND ANTHROPOGENIC OSMIUM IN LONG-ISLAND SOUND, AN URBAN ESTUARY IN THE EASTERN US, Earth and planetary science letters, 148(1-2), 1997, pp. 341-347
The Os concentration and Os-187/Os-186 distributions in surface sedime
nts of Long Island Sound (eastern U.S.) provide a way of determining t
he sources and estuarine transport of Os. The contribution of anthropo
genic Os from sewer outfalls from the New York City region supplies a
tracer with a characteristic Os-187/Os-186 Of about 1. The Os concentr
ation of the bulk surface sediment increases steeply moving toward New
York City in the westernmost Sound and generally follows the concentr
ation of organic carbon, The Os-187/Os-186 ratio of bulk surface sedim
ent increases from west to east in the westernmost part of the Sound a
nd is effectively constant in the central Sound. We interpret these re
sults as indicating that the surface bulk sediments of the Sound conta
in a low Os-187/Os-186 component, perhaps as a reduced coating associa
ted with organic remains from sewer outfalls. The acid hydrogen peroxi
de leach fraction has an average Os-187/Os-186 of 9.5 in the central S
ound, significantly higher than both the bulk sediment value and the p
robable sea water value of about 8. The leach fraction in thr westernm
ost part of the traverse is less radiogenic than the central Sound and
follows the Os isotope trend of the bulk sediment. Liquid effluent fr
om a New York City sewer outfall contains 30 pg l(-1) of dissolved Os
with a Os-187/Os-186 of about 2.5, consistent with its being an end-me
mber of the west-east sediment pattern recorded in the leach fractions
of the westernmost cores. The leachable Os from the central Sound pre
dominantly reflects Os in ferromanganese oxyhydroxide coatings from co
ntinentally derived sediments with Os-187/Os-186 ratios more radiogeni
c than seawater. The distribution patterns of anthropogenic and natura
l Os, with their characteristic isotopic signatures in the Sound, and
the insights gained from the behavior of other particle-reactive speci
es, indicates that very little Os in solution may pass through the est
uarine gauntlet.