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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.
Kazumi Asahi, Masao Kitamura, Eishi Ibe, Yamato Asakura, Shunsuke Uchida
Nuclear Science and Engineering | Volume 95 | Number 4 | April 1987 | Pages 257-265
Technical Paper | doi.org/10.13182/NSE87-A20437
Articles are hosted by Taylor and Francis Online.
Double oxide layers were observed on the stainless steel coupons. The outer layer consisted of well-developed crystals (diameter: 0.5 to 1.0 üm, probable major oxide form: NiO Fe2O3), while the inner layer consisted of smaller particles [diameter: 0.1 to 0.3 μm, probable major oxide form: NiO-(Cr,Fe)2O3]. The depletion of chromium and nickel and the accumulation of impurities in the water, such as 60Co, zinc, and copper, were observed in the outer layer. For the carbon steel the chromium-rich layer existed at the outer/inner interface. It was considered that the outer and inner layers were a corundum-type oxide (Cr,Fe)2O3. The outer layer seemed to be formed by a wet corrosion mechanism (dissolution-precipitation of metal), while the inner layer seemed to be formed by a dry corrosion one (reaction of metal with oxygen diffused through the oxide layers from the water). More than 80% of the 60Co in a coupon was included in the outer layer, and it was supposed that this was deposited mainly during wet corrosion.