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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.
F. C. Schoenig, K. S. Quisenberry, D. P. Stricos, and H. Bernatowicz
Nuclear Science and Engineering | Volume 26 | Number 3 | November 1966 | Pages 393-398
Technical Paper | doi.org/10.13182/NSE66-A17362
Articles are hosted by Taylor and Francis Online.
The temperature dependence of the thorium-oxide resonance integral has been measured over a wide (20 to 1550 °C) temperature range. The activation method was used; the 310 keV γ ray from the decay of 233Pa was measured with a multichannel pulse-height analyzer. Measurements were performed on ThO2 rods of 0.490− and 0.353−in. diam. (surface-to-mass ratio = 0.340 and 0.465 cm2/g, respectively). The temperature dependence of the thorium-oxide resonance integral was found not to be a linear function of either (t − t0) or (√T − √T0), where t and T and centigrade and Kelvin temperature, and t0 and T0 are 20°C, and 293°K, respectively. Thus the familiar forms of the temperature dependence of the effective resonance integral, namely RI(T)/RI(T0) = 1 + α (t − t0) = 1 + β × (√T − √To) are not appropriate representations of the data. The Doppler coefficient in a 1/E spectrum is defined by α0 = [1/RI(T)] [dRI(T)/ dT] where RI(T) is the effective resonance integral of the sample excluding the 1/v contribution, and T is the temperature of the sample. It has been found that α0 = [(0.16 ± 0.01)/T] yields a good fit to the experimental data of both sample sizes. It follows that RI(T) = RI(T0) (T/T0)(0.16 ± 0.01).