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Bien, G. S.; Rakestraw, N. W.; Suess, H. E. (2011)
Publisher: Co-Action Publishing
Journal: Tellus A
Languages: English
Types: Article
Results of C14 determinations in surface water from the Pacific were in agreement with those reported by Rafter and Fergusson. However, abnormal C14 concentrations seem to exist locally, for which no oceanographic explanation can be given. It seems premature to draw conclusions from existing determinations as to the rate of increase of C14 in surface ocean water resulting from the uptake of C14 produced in the atmosphere by atomic bombs. Samples from a constant depth of about 3,500 meters show a C14 content decreasing from south to north. This decrease may be attributed to radioactive decay of C14 during the time of migration. From this the northward component of the rate of water movement of about 0.06 cm/sec can be calculated. The C13 determinations, for the purpose of correcting the C14 values for isotope fractionation effects, were found to be remarkably consistent, although made on reburned acetylene.DOI: 10.1111/j.2153-3490.1960.tb01330.x
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    • ARNOLDJ., R. and ANDERSOEN., C., 1957: The Distribution of C-14 in Nature, Tellus 9, pp. 28-32.
    • BROBCKEWR, . S. and WALTONA,., 1959: Radiocarbon From Nuclear Tests, Science 130, p. 309.
    • BROECKBRW, . S., TUCEKC,. S. and OLWONE,. A., 1959: Radiocarbon Analysis of Oceanic CO,, International Journal of Applied Radiation and Isotopes.
    • BURLINGR,. W. and GARNERD, . M., 1959: A Section of I4C Activities of Sea Water Between g"S and 60° S in the Southwest Pacific Ocean, N.Z. Journal Geology and Geophysics, 2, p. 799.
    • CRAIG,H., 1957: The Natural Distribution of Radiocarbon and the Exchange Time of Carbon Dioxide Between Atmosphere and Sea, Tellus 9. pp. 1-17.
    • -, 1957: Isotopic Standards for Carbon and Oxygen and Correction Factors for Mass-Spectrometric Analysis of Carbon Dioxide, Geochim. et Cosmochim . h l , 12, p. 133.
    • FERGUSSONG,. J., 1958: Reduction of atmospheric Radiocarbon Concentration by Fossil Fuel Carbon. Dioxide and the Mean Life of Carbon Dioxide in the Atmosphere, Proceedings Royal Society, A234. pp. 561-74.
    • HONTERMANFS.,G. and OESCHGEHR,., 1958: A Special Low-Level Counter, Helvetica Physira Arta, 31, p. 117.
    • RAFTER, T. A. and FERGUSSOGN., J., 1900: Atmospheric Radiocarbon as a Tracer in Geophysical Circulation Problems, N.Z. Journal of Science and Technology. B38.
    • REVELLBR,. and SUESS,H. E., 1957: Carbon Dioxide Exchange Beetwen Atmosphere and Ocean and the Question of an Increase of Atmospheric C 0 2during the Past Decade., Tellus, 9, pp. 18-27.
    • SUESSH,. E., 1954: Natural Radiocarbon Measurements by Acetylene Counting., Science, 120, pp. 5-6.
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