Abstract
Volkova and Zatsepin1 were the first to propose the use of a ‘Tevatron’ (a high-energy accelerator at 1012 eV or TeV energies) to beam neutrinos v through the Earth to a mobile detector and obtain X rays of the planet's interior. The basic idea has been contingent for years on the opacity of the Earth to neutrinos at appropriate energies (10–103 TeV). This depends significantly on the neutrino–nucleon scattering cross-section, which in turn depends on the existence of an intermediate vector boson2–4, the acceptance of what physicists refer to as the standard model5–7 in high-energy physics, and finally the mass MW of the intermediate W boson in that model. The announcement by CERN of the W boson mass8,9 (MW ∼80 GeV) permits us now to draw certain conclusions. Although we shall demonstrate that neutrino tomography at planetary densities is feasible, tomographic scanning schemes appear unrealistic in several respects. We shall address two sources of neutrinos for tomographic mapping of the densities, the Earth-based Tevatron and the neutrino sky.
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Wilson, T. Neutrino tomography: Tevatron mapping versus the neutrino sky. Nature 309, 38–42 (1984). https://doi.org/10.1038/309038a0
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DOI: https://doi.org/10.1038/309038a0
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