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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.
N. S. Klimov, V. A. Kurnaev, A. M. Zhitlukhin, D. V. Kovalenko, I. M. Poznyak, A. A. Moskacheva, D. B. Abramenko
Fusion Science and Technology | Volume 60 | Number 1 | July 2011 | Pages 34-39
doi.org/10.13182/FST11-A12402
Articles are hosted by Taylor and Francis Online.
The paper concerns experimental investigations of metallic material erosion under the plasma heat loads expected in ITER divertor during transient events such as the type I edge-localized modes and the disruptions. Primary attention is focused on the erosion due to melt layer movement and splashing. The targets of tungsten and other metals were repeatedly exposed to hydrogen plasma flow of 0.5 ms duration in the heat load range of 0.2-4.5 MJ/m2 at the TRINITI plasma gun QSPA-T. The ejection of liquid droplets was observed during plasma exposure by special recoded system and onset conditions of droplets ejection were defined. Between some of the plasma pulses the eroded surface was analyzed with profilometry and microscopy. The mass loss and exposed surface profile were measured as a function of heat load and number of pulses. Experimentally measured target thinning due to melt layer removal from the exposed area to periphery was compared with erosion due to mass loss as a result of droplets ejection and evaporation. The obtained surface profile was compared with the result of numerical calculations which based on simultaneous solving of the 2-D heat conductivity equation and hydrodynamics equations of “shallow water” approximation.