Mathematics – Logic
Scientific paper
Apr 1994
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1994gecoa..58.1795w&link_type=abstract
Geochimica et Cosmochimica Acta, vol. 58, Issue 7, pp.1795-1811
Mathematics
Logic
7
Scientific paper
Vertical profiles of dissolved and particulate 210 Pb and 210 Po were determined at two stations in the Black Sea in June 1988. Vertical fluxes of 210 Pb and 210 Po were also measured in the upper 150 m, using floating sediment traps. The fractionation of 210 Pb between dissolved and particulate phases in the Black Sea is strongly influenced by the redox conditions in the water column. Dissolved 210 Pb dominates in the oxic zone, while particulate 210 Pb is the major form in the deep sulfide-rich anoxic zone. The distribution of 210 Pb across the suboxic zone appears to be mainly controlled by redox cycling of manganese and iron. In the sulfide-rich layer coprecipitation of lead with iron sulfide is probably the dominant scavenging mechanism. A simple scavenging model was used to calculate the residence times of dissolved and particulate 210 Pb in the oxic, suboxic, and anoxic zones. The residence times of dissolved 210 Pb relative to scavenging by particles are 0.5-1, 2-3, and 3.5 years in the oxic, suboxic, and anoxic layers, respectively. The corresponding residence times of particulate 210 Pb relative to particle removal processes in the same layers are 0.1, 1.5-2.5, and 8.5 years, respectively. A particle settling velocity of about 40 m y -1 was derived from the 210 Pb / 226 Ra disequilibrium in the deep Black Sea. The relatively short residence times of 210 Pb support the hypothesis that anoxic basins are important sites for boundary scavenging of 210 Pb. The 210 Po profiles indicate that biological rather than inorganic particles are the major carrier phases for polonium in the Black sea. Dissolved 210 Po is deficient relative to dissolved 210 Pb in the euphotic zone, suggesting preferential uptake of 210 Po over 210 Pb by particles residing in that layer. The residence time of dissolved 210 Po, with respect to scavenging by particles in the euphotic zone, is about 200 days. Below the mid-depth of the suboxic zone, 210 Po is in excess relative to 210 Pb, and is thought to originate from shelf and slope sediments. Based on the magnitude of distribution coefficients ( K D ), the relative partitioning of lead, polonium, and thorium to particles found in the oxic and anoxic layers of the Black Sea are Po > Th > Pb and Po = Pb > Th, respectively. The dependency of K D on particle concentration suggests that colloidal phases may be important for the scavenging of these radionuclides.
Murray James W.
Wei Ching-Ling
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