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- W2015444608 abstract "Anaerobic sediments from the upper continental slope in the eastern Pacific, the Gulf of California, and a Norwegian Fjord have been analyzed for their total uranium content and 234U/238U ratios by alpha-spectrometry. The uranium concentrations range from 4.8 to 39 ppm and are thus significantly higher than the average uranium content of 3 ppm in deep sea clays, stream sediments and soils. The 234U/238U ratios approach the sea water value of 1.15 in samples with high uranium content. These results indicate that uranium is being removed from sea water in near shore areas under certain conditions. If such conditions prevail in only 0.4% of the total area covered by the ocean, an amount of uranium equal to that supplied by streams (assuming 0.04 μg/ℓ) can be removed from the ocean, on the basis of measured accumulation rates in the Gulf of California, off southern California, and in other areas. The effect of Pleistocene sea level fluctuations as a controlling factor in determining the concentration of uranium in sea water is diminished by the occurrence of extensive areas of uranium deposition below 200 m and by the very long residence time of uranium in the ocean." @default.
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- W2015444608 date "1967-01-01" @default.
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- W2015444608 title "Deposition of uranium from the ocean" @default.
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- W2015444608 doi "https://doi.org/10.1016/0012-821x(67)90026-x" @default.
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