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Conference Spotlight
Nuclear Energy Conference & Expo (NECX)
September 8–11, 2025
Atlanta, GA|Atlanta Marriott Marquis
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Hash Hashemian: Visionary leadership
As Dr. Hashem M. “Hash” Hashemian prepares to step into his term as President of the American Nuclear Society, he is clear that he wants to make the most of this unique moment.
A groundswell in public approval of nuclear is finding a home in growing governmental support that is backed by a tailwind of technological innovation. “Now is a good time to be in nuclear,” Hashemian said, as he explained the criticality of this moment and what he hoped to accomplish as president.
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.