Abstract
Three classes of radioactive nuclear species that occur on the surface of the Earth have been determined: (1) extremely long lived species that have surivved from the time when the elements were formed (primary radionuclides) and their daughter products (secondary radionuclides); (2) radioactive nuclei that are currently formed in nature, primarily by cosmic ray induced processes; (3) man-made radioactive substances, such as those produced through the testing of atomic devices or in nuclear reactors. This paper gives a brief account of the nature of geochemical, meteorological, and oceanographic problems involve din the interpretation of the distribution of radioactivity in the atmosphere and the hydrosphere of the earth.
Cite
CITATION STYLE
Lal, D., & Suess, H. E. (1968). The Radioactivity of the Atmosphere and Hydrosphere. Annual Review of Nuclear Science, 18(1), 407–434. https://doi.org/10.1146/annurev.ns.18.120168.002203
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