<HashMap><database>biostudies-literature</database><scores/><additional><omics_type>Unknown</omics_type><volume>334(12)</volume><submitter>Joyce MJ</submitter><pubmed_abstract>Measurements of refractory and volatile components in soils from Northern England confirm &lt;sup>244&lt;/sup>Pu/&lt;sup>239&lt;/sup>Pu consistent with the global average but refractory &lt;sup>240&lt;/sup>Pu/&lt;sup>239&lt;/sup>Pu 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 &lt;sup>240&lt;/sup>Pu/&lt;sup>239&lt;/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 &lt;sup>239&lt;/sup>Pu fission and capture cross-section enhancement due to the S-wave resonance at ~ 0.3 eV. A further calibration with a &lt;sup>240&lt;/sup>Pu standard is recommended to substantiate these observations.&lt;h4>Supplementary information&lt;/h4>The online version contains supplementary material available at 10.1007/s10967-025-10541-0.</pubmed_abstract><journal>Journal of radioanalytical and nuclear chemistry</journal><pagination>9287-9299</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC12827445</full_dataset_link><repository>biostudies-literature</repository><pubmed_title>Plutonium signatures in refractory fallout support a Chernobyl nuclear jet hypothesis.</pubmed_title><pmcid>PMC12827445</pmcid><pubmed_authors>Gautschi P</pubmed_authors><pubmed_authors>Joyce MJ</pubmed_authors><pubmed_authors>Collins-Price P</pubmed_authors><pubmed_authors>Livens F</pubmed_authors><pubmed_authors>Wilbraham R</pubmed_authors><pubmed_authors>Warwick P</pubmed_authors><pubmed_authors>Gaca P</pubmed_authors><pubmed_authors>Semple KT</pubmed_authors><pubmed_authors>Boxall C</pubmed_authors><pubmed_authors>Madina A</pubmed_authors><pubmed_authors>Christl M</pubmed_authors></additional><is_claimable>false</is_claimable><name>Plutonium signatures in refractory fallout support a Chernobyl nuclear jet hypothesis.</name><description>Measurements of refractory and volatile components in soils from Northern England confirm &lt;sup>244&lt;/sup>Pu/&lt;sup>239&lt;/sup>Pu consistent with the global average but refractory &lt;sup>240&lt;/sup>Pu/&lt;sup>239&lt;/sup>Pu 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 &lt;sup>240&lt;/sup>Pu/&lt;sup>239&lt;/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 &lt;sup>239&lt;/sup>Pu fission and capture cross-section enhancement due to the S-wave resonance at ~ 0.3 eV. A further calibration with a &lt;sup>240&lt;/sup>Pu standard is recommended to substantiate these observations.&lt;h4>Supplementary information&lt;/h4>The online version contains supplementary material available at 10.1007/s10967-025-10541-0.</description><dates><release>2025-01-01T00:00:00Z</release><publication>2025</publication><modification>2026-06-06T22:29:08.238Z</modification><creation>2026-06-06T03:10:38.966Z</creation></dates><accession>S-EPMC12827445</accession><cross_references><pubmed>41586250</pubmed><doi>10.1007/s10967-025-10541-0</doi></cross_references></HashMap>