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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.
Carl H. Distenfeld and Robert D. Colvett
Nuclear Science and Engineering | Volume 26 | Number 1 | September 1966 | Pages 117-121
Technical Paper | doi.org/10.13182/NSE66-A17194
Articles are hosted by Taylor and Francis Online.
The Special Measurements Group at the Brookhaven Alternating Gradient Synchrotron has conducted detailed experiments to evaluate and understand radiations emanating from the accelerator. As a part of this group study, skyshine and attenuation through Long Island sand was measured. Attenuation 90° from the apparent line source followed a half thickness of about one foot of sand through at least four decades. This corresponds to an attenuation length in sand of 80 g/cm2., Skyshine was measured out to 1000 m from the target. The empirical results fit the following expression for 4.2 × 1011 protons/sec on target: I = (3000/r2) exp(-r/600) [1 - exp(r/47)] where I is the dose rate in mrem/h and r is the source detector distance in meters. The source luminosity was determined, and a skyshine function was derived, based on the luminosity and the expected attenuation in air based on sand results. The empirical function was found to be within 25% of the derived expression.