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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.
Mildred J. Bradley, Jerry H. Goode, Leslie M. Ferris, James R. Flanary and Jacob W. Ullmann
Nuclear Science and Engineering | Volume 21 | Number 2 | February 1965 | Pages 159-164
Technical Paper | doi.org/10.13182/NSE65-A21039
Articles are hosted by Taylor and Francis Online.
Reactor irradiation of uranium monocarbide (UC) caused pronounced effects on its reactions with water and with aqueous solutions of NaOH, HCl, and H2SO4. Specimens irradiated to a burnup of 0.6 at.% or higher were essentially inert to water and to 6 M NaOH at 80°C. When the burnup was 0.06 at.% the specimens hydrolyzed, but the rates were much lower than those obtained with unirradiated specimens. The irradiation had little effect on the rates of reaction with HCl and H2SO4. When hydrolysis of irradiated UC occurred in water, 6 M NaOH, 6 M HCl, or 6 M H2SO4, the gases evolved contained less methane, less total volatile hydrocarbons and more hydrogen than the gases evolved from unirradiated UC under the same conditions. In general, with increasing burnup of the UC, the amount of hydrogen evolved increased while the amounts of methane and total carbon recovered in the gas decreased.