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Uranium-233

Isotope of uranium

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Through Alpha decay, Half-life and Neutron

Uranium-233 is produced by the neutron irradiation of thorium-232. When thorium-232 absorbs a neutron, it becomes thorium-233, which has a half-life of about 22 minutes. Thorium-233 decays into protactinium-233 through beta decay. Protactinium-233 has a longer half-life of about 27 days to further decay into uranium-233; some proposed molten salt reactor designs attempt to physically isolate the protactinium from further neutron capture before beta decay can occur, to maintain the neutron economy.

233U usually fissions on neutron absorption, but sometimes retains the neutron, becoming uranium-234. At a neutron energy of 0.0253 eV, JENDL-4.0 data give capture-to-fission ratios of about 0.085 for uranium-233, 0.169 for uranium-235 and 0.363 for plutonium-239.

History

The fissile properties of uranium-233 were established at the University of California, Berkeley during 1941 and early 1942 by Glenn T. Seaborg, John W. Gofman and Raymond W. Stoughton, who showed that the isotope undergoes fission with slow neutrons and was therefore a potential nuclear fuel. Their report was mailed to the Uranium Committee in Washington on 14 April 1942, but wartime secrecy kept the work from open publication until 1947, when an abridged version appeared in Physical Review.

In 1946, the public first became informed of uranium-233 bred from thorium as "a third available source of nuclear energy and atom bombs" (in addition to uranium-235 and plutonium-239), following a United Nations report and a speech by Glenn T. Seaborg.

The United States produced, over the course of the Cold War, approximately 2 metric tons of uranium-233, in varying levels of chemical and isotopic purity. These were produced at the Hanford Site and Savannah River Site in reactors that were designed for the production of plutonium-239.

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