210 Pb-derived chronology and the fluxes of 210 Pb and 137 Cs isotopes into continental shelf sediments, East Chukchi Sea, Alaskan Arctic

Details 210 Pb-derived chronology and the fluxes of 210 Pb and 137 Cs isotopes into continental shelf sediments, East Chukchi Sea, Alaskan Arctic 210 Pb-derived chronology and the fluxes of 210 Pb and 137 Cs isotopes into continental shelf sediments, East Chukchi Sea, Alaskan Arctic

Nov 1995

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1995gecoa..59.4435b&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 59, Issue 21, pp.4435-4448

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9

Scientific paper

Eleven sediment cores and eight sediment trap samples from the continental shelf of the Eastern Chukchi Sea were analyzed for 210Pb, Cs, and 2226Ra. In selected samples, the organic carbon content and stable carbon isotope ratios were also determined. The excess 210 Pb ( 210 Pb xs ) concentrations in the 1-cm core tops are generally lower than those of surficial sediments of subarctic shelves and arctic lakes. The sediment inventory-derived depositional fluxes of 210 Ph vary between 0.09 and 0.38 dpm cm -2 y-1 , with a mean of 0.18 dpm cm -2 y -1 . The apparent mass sediment accumulation rates, which vary between 31 and 324 mg cm -2 y -1 with a mean value of 133 mg cm -2 y -1 , are about an order of magnitude lower than the yearly particle flux obtained from the sediment trap experiments. This difference between the relatively long-term and short-term yearly accumulation rates is likely due to the occasional resuspension of fine particles in the continental shelf areas and their advective transport to sites other than their initial deposition. The sediment inventory of 137 Cs varied between 0.64 and 4.09 dpm cm -2 , with a mean of 2.18 dpm cm -2 . A comparison of this inventory with the expected fallout inventory of 137 Cs suggests that there had been no detectable input of 137 Cs to the study area from the former USSR nuclear dump sites.

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