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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.
Marvin Tetenbaum, Larry Mishler, Glenn Schnizlein
Nuclear Science and Engineering | Volume 14 | Number 3 | November 1962 | Pages 230-238
doi.org/10.13182/NSE62-A26211
Articles are hosted by Taylor and Francis Online.
Because ignition temperature is not an intrinsic property of a substance, the investigation reported in this paper was undertaken to measure the ignition behavior of uranium powder under well-defined boundary conditions such that quantitative predictions are possible. The ignition behavior of uranium powder has been found to be dependent on specific area of powder fraction, rate of heating, and geometry of sample. For a given mesh size powder and heating rate, constant limiting ignition temperature values are obtained practically independent of container size, when the powder bed exceeds a critical height. Critical height values are found to increase with particle size of powder; for a given particle size powder, critical height values decrease with heating rate. On the basis of the Frank-Kamenetskii theory of thermal explosions, when used in a restricted manner, limiting ignition temperature values for uranium powder can be estimated using critical height values as the significant geometrical dimension of the container. These calculated ignition temperatures are in reasonable agreement with those obtained with our experimental apparatus. The ignition behavior of uranium powder can be adequately described by converting isothermal expressions to a rising temperature basis according to the treatment of Murray, Buddery, and Taylor.