233U/236U signature allows to distinguish environmental emissions of civil nuclear industry from weapons fallout

K. Hain (), P. Steier, M. B. Froehlich, R. Golser, X. Hou, J. Lachner, T. Nomura, J. Qiao, F. Quinto and A. Sakaguchi
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K. Hain: Faculty of Physics, Isotope Physics, University of Vienna
P. Steier: Faculty of Physics, Isotope Physics, University of Vienna
M. B. Froehlich: Australian National University
R. Golser: Faculty of Physics, Isotope Physics, University of Vienna
X. Hou: Technical University of Denmark
J. Lachner: Faculty of Physics, Isotope Physics, University of Vienna
T. Nomura: Graduate School of Science, Hiroshima University
J. Qiao: Technical University of Denmark
F. Quinto: Karlsruhe Institute of Technology (KIT), Institute for Nuclear Waste Disposal (INE)
A. Sakaguchi: University of Tsukuba

Nature Communications, 2020, vol. 11, issue 1, 1-11

Abstract: Abstract Isotopic ratios of radioactive releases into the environment are useful signatures for contamination source assessment. Uranium is known to behave conservatively in sea water so that a ratio of uranium trace isotopes may serve as a superior oceanographic tracer. Here we present data on the atomic $$^{233}$$233U/$$^{236}$$236U ratio analyzed in representative environmental samples finding ratios of (0.1–3.7)$$\cdot$$⋅10$$^{-2}$$−2. The ratios detected in compartments of the environment affected by releases of nuclear power production or by weapons fallout differ by one order of magnitude. Significant amounts of $$^{233}$$233U were only released in nuclear weapons fallout, either produced by fast neutron reactions or directly by $$^{233}$$233U-fueled devices. This makes the $$^{233}$$233U/$$^{236}$$236U ratio a promising new fingerprint for radioactive emissions. Our findings indicate a higher release of $$^{233}$$233U by nuclear weapons tests before the maximum of global fallout in 1963, setting constraints on the design of the nuclear weapons employed.

Date: 2020
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DOI: 10.1038/s41467-020-15008-2

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