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Conference Spotlight
Nuclear Energy Conference & Expo (NECX)
September 8–11, 2025
Atlanta, GA|Atlanta Marriott Marquis
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The RAIN scale: A good intention that falls short
Radiation protection specialists agree that clear communication of radiation risks remains a vexing challenge that cannot be solved solely by finding new ways to convey technical information.
Earlier this year, an article in Nuclear News described a new radiation risk communication tool, known as the Radiation Index, or, RAIN (“Let it RAIN: A new approach to radiation communication,” NN, Jan. 2025, p. 36). The authors of the article created the RAIN scale to improve radiation risk communication to the general public who are not well-versed in important aspects of radiation exposures, including radiation dose quantities, units, and values; associated health consequences; and the benefits derived from radiation exposures.
W. Zobel, F. C. Maienschein, J. H. Todd, and G. T. Chapman
Nuclear Science and Engineering | Volume 32 | Number 3 | June 1968 | Pages 392-406
Technical Paper | doi.org/10.13182/NSE68-A20222
Articles are hosted by Taylor and Francis Online.
Determining the contribution of secondary gamma rays to the radiation dose produced by charged particles in space requires a knowledge of the cross sections for gamma-ray production by protons and alpha particles. The only data of this type that have been available have been for ∼145-MeV protons. In the experiment reported here, gamma-ray spectral measurements were made for protons of 16, 33, 56, and 160 MeV and alpha particles of 59 MeV incident on targets of low- and medium-Z materials. Absolute spectra were obtained, generally in the backward direction, with coincidence (pair) or anticoincidence (total-absorption) scintillation spectrometers. The analysis method used to correct for the imperfect spectrometer response yielded quantitative error estimates for the resultant spectra. A few measurements were made in the forward direction or at 90° to distinguish deviations from isotropy which were marked only for 16-MeV protons incident on a carbon target. From the spectra, cross sections were obtained for the production of specific gamma rays. Tables of these results include the probable nuclear reactions which produced the gamma rays. The production cross sections are plotted vs the average proton energy in the target for individual gamma rays for C and O. For each element, these individual production cross sections are added and the sums, which decrease with increasing proton energy, are compared with the total nonelastic cross sections predicted on the basis of intranuclear cascade calculations. The reasonably smooth variations of the total cross sections for gamma-ray production with atomic number are also shown. The proton inelastic scattering cross sections for specific levels correspond within error to 14-MeV neutron scattering data.