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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.
Clay A. Cooper, David L. Decker
Nuclear Technology | Volume 174 | Number 3 | June 2011 | Pages 452-459
Technical Paper | TOUGH2 Symposium / Radioactive Waste Management and Disposal | doi.org/10.13182/NT11-A11752
Articles are hosted by Taylor and Francis Online.
Nuclear rocket engine technology is being considered as a means of interplanetary vehicle propulsion for a manned mission to Mars. Significant technological research and development are required before nuclear-based rocket propulsion can be integrated into an interplanetary vehicle, including the firing of full-scale nuclear rocket engines in a test and evaluation facility. Testing of nuclear engines in the 1950s and 1960s was accomplished by directing engine exhaust gases into the atmosphere, a practice that is no longer acceptable. Testing nuclear rocket engines by injection of associated radioactive exhaust gases and water vapor into deep unsaturated zones may be a way to sequester radionuclides and will require comprehensive design of a nuclear engine test facility. We conducted numerical simulations to determine the ability of an unsaturated zone with the hydraulic properties of Yucca Flat alluvium at the Nevada National Security Site to contain gas-phase radionuclides. In these simulations, gas and water vapor (from water sprayed into the exhaust for cooling) were injected for two hours at a temperature of 600°C and with rates of 14.5 kg s-1 and 15 kg s-1 , respectively, in varying thicknesses of alluvium with an intrinsic permeability of 10-11 m2 and porosity of 0.35. These simulations suggest that following the test of an engine, gaseous radionuclides injected below 200 m will not migrate to the land surface. The simulations show that the gaseous/vapor injectate will cool and condense within several meters of the injection point, although there will be limited, if any, downward drainage of liquid. However, the nearly horizontal hydraulic groundwater gradient present in Yucca Flat should limit lateral migration of any condensate that may drain downward and reach the water table.