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Conference Spotlight
2025 ANS Winter Conference & Expo
November 8–12, 2025
Washington, DC|Washington Hilton
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Latest News
Japan gets new U for enrichment as global power and fuel plans grow
President Trump is in Japan today, with a visit with new Prime Minister Sanae Takaichi on the agenda. Takaichi, who took office just last week as Japan’s first female prime minister, has already spoken in favor of nuclear energy and of accelerating the restart of Japan’s long-shuttered power reactors, as Reuters and others have reported. Much of the uranium to power those reactors will be enriched at Japan’s lone enrichment facility—part of Japan Nuclear Fuel Ltd.’s Rokkasho fuel complex—which accepted its first delivery of fresh uranium hexafluoride (UF₆) in 11 years earlier this month.
A. D. Whapham
Nuclear Technology | Volume 2 | Number 2 | April 1966 | Pages 123-130
Technical Paper | doi.org/10.13182/NT66-A27492
Articles are hosted by Taylor and Francis Online.
The structure of post-irradiation annealed UO2 has been examined by transmission electron microscopy to try to understand the behavior and release of fission gas. At a dose of 2.2 × 1019 fissions/cm3, 5 × 1015 small gas bubbles/cm3 are observed in the material. These precipitate at 1100°C and appear to grow from 25 to 100-Å diam at 1500°C by diffusion of gas atoms from the matrix. Grain-boundary migration sweeps up these bubbles at between 1800 and 2000°C. Re-solution of fission-gas bubbles up to 300-Å diam has been demonstrated on re-irradiation. At a dose of 1.6 × 1020 fissions/cm3, bubbles appear to grow by coalescence and by dislocation sweeping. Precipitates, believed to be solid fission products, are observed. It is concluded that, in a fuel element in which a high-temperature gradient exists, the gas release below 1800°C will be controlled by the migration of bubbles to grain boundaries and by the degree of linking up between the gas-filled voids produced at grain boundaries. At temperatures above 1800°C, large gas-filled voids produced at grain boundaries would be expected to migrate up the temperature gradient by the vapor-transfer mechanism, continuing the process of sweeping up most of the gas started by the initial grown-in porosity.