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Going Nuclear: Notes from the officially unofficial book tour
I work in the analytical labs at one of Europe’s oldest and largest nuclear sites: Sellafield, in northwestern England. I spend my days at the fume hood front, pipette in one hand and radiation probe in the other (and dosimeter pinned to my chest, of course). Outside the lab, I have a second job: I moonlight as a writer and public speaker. My new popular science book—Going Nuclear: How the Atom Will Save the World—came out last summer, and it feels like my life has been running at full power ever since.
D. A. Powers
Nuclear Science and Engineering | Volume 88 | Number 3 | November 1984 | Pages 357-366
Technical Paper | doi.org/10.13182/NSE84-A18589
Articles are hosted by Taylor and Francis Online.
Molten stainless steel at ∼1720°C and melts of iron and alumina or 54 wt% UO2, 16 wt% ZrO2, and 30 wt% stainless steel at 2400 to 2800°C were poured onto 0.95- to 7.62-cm-thick steel structures. The melts rapidly penetrated these structures, probably by a thermal ablation process. Coatings of 0.2- to 2-mm-thick urania on the surfaces of the steel delayed penetration by the very high-temperature melts. Data from tests involving melts impinging on steel structures could be correlated by the single-parameter, empirical expression A finite difference model of the experiments is described. The model is used as the basis for predicting the extent of crust formation when melts contact cold steel and to suggest that a gas gap may form between the steel and any crust of frozen material that does form.