<p>Measurements of refractory and volatile components in soils from Northern England confirm <sup>244</sup>Pu/<sup>239</sup>Pu consistent with the global average but refractory <sup>240</sup>Pu/<sup>239</sup>Pu significantly higher but consistent with Chernobyl fallout, i.e., 0.390 ± 0.006. Refractory formation suggests temperatures &gt; 3000°C, consistent with atmospheric injection by nuclear-driven explosions rather than &#xa0;by&#xa0;steam or hydrogen. Volatile <sup>240</sup>Pu/<sup>239</sup>Pu is consistent with the global average, 0.181 ± 0.002, and hence lower-temperature formation in the chemical explosions and subsequent fire. This hypothesis is supported by <sup>239</sup>Pu fission and capture cross-section enhancement due to the S-wave resonance at ~ 0.3&#xa0;eV. A further calibration with a <sup>240</sup>Pu standard is recommended to substantiate these observations.</p>

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Plutonium signatures in refractory fallout support a Chernobyl nuclear jet hypothesis

  • Malcolm. J. Joyce,
  • Colin Boxall,
  • Marcus Christl,
  • Patrick Collins-Price,
  • Pawel Gaca,
  • Philip Gautschi,
  • Francis Livens,
  • Argaia Madina,
  • Kirk T. Semple,
  • Phillip Warwick,
  • Richard Wilbraham

摘要

Measurements of refractory and volatile components in soils from Northern England confirm 244Pu/239Pu consistent with the global average but refractory 240Pu/239Pu significantly higher but consistent with Chernobyl fallout, i.e., 0.390 ± 0.006. Refractory formation suggests temperatures > 3000°C, consistent with atmospheric injection by nuclear-driven explosions rather than  by steam or hydrogen. Volatile 240Pu/239Pu is consistent with the global average, 0.181 ± 0.002, and hence lower-temperature formation in the chemical explosions and subsequent fire. This hypothesis is supported by 239Pu fission and capture cross-section enhancement due to the S-wave resonance at ~ 0.3 eV. A further calibration with a 240Pu standard is recommended to substantiate these observations.