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• W2014732856 abstract "In 1977 and 1981 a hydrothermal plume was detected at the East Pacific Rise (EPR) near 8°45′N and at MANOP Site M, 25 km east of the EPR, by anomalous222Rn and Mn concentrations. In 1981, samples were also taken for210Pb,210Po and226Ra analyses to determine if enhanced scavenging of these elements occurred in the plume. At both the ridge crest and at Site M, the 210Pb/226Ra ratios range from 0.09 to 0.35, which are among the lowest values ever measured. It appears that removal of the210Pb is occurring by processes operating at or near the seafloor. There is also significant 210Po/210Pb disequilibrium at both locations, which appears to increase away from the seafloor towards the plume (as indicated by elevated Mn concentrations). An in-situ water column scavenging process is suggested by correlation of [210Pb-210Po] and Mn concentrations in the plume. The residence time of the210Po is only about 1 year, which is close to its residence time in surface waters but quite short compared to typical deep sea values. Thus rapid scavenging of the polonium in the plume and relatively rapid settling of particles from the plume is suggested." @default.
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• W2014732856 date "1987-02-01" @default.
• W2014732856 modified "2023-09-26" @default.
• W2014732856 title "Enhanced scavenging of210Pb and210Po by processes associated with the East Pacific Rise near 8°45′N" @default.
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• W2014732856 doi "https://doi.org/10.1016/0012-821x(87)90122-1" @default.
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