DETERMINATION OF PU ISOTOPE SYSTEMATICS OF TRINITITE POST-DETONATION MATERIAL
Trinitite is the blast melt that resulted from the world’s first atomic test at the Trinity site, near Alamogordo, New Mexico (05:29:45AM on July 16th, 1945). The Trinity device was an implosion-type device organized in several concentric shells and containing about 6 kg of supergrade Pu fuel (~99.1% of 239Pu, ~0.9% of 240Pu and trace amounts of 241Pu). The lack of a commercially available Pu isotope standard for use as an external calibration standard to monitor instrumental mass bias during LA-MC-ICP-MS analyses is somewhat problematical. However, the latter was monitored using a ‘standard-sample’ bracketing technique measuring the 235U/238U ratio for the NIST SRM 610 standard glass wafer. Ion signals for 239Pu, 240Pu, and 241Pu (+ 241Am) were collected simultaneously by three ion counters. Prior to laser ablation analysis, the efficiency for each ion counter was assessed by measuring the Pb isotope ratios for solutions of varying concentrations (ppb level) of the NIST SRM 981 standard. The laser ablation data indicates that areas within Trinitite characterized by high 239Pu ion signals record 240Pu/239Pu ratios between 0.025 and 0.035, whereas regions that yield much lower 239Pu signals are associated with higher 240Pu/239Pu ratios. Similar trends were also recorded for laser ablation analyses conducted with a high-resolution-ICP-MS instrument. The combined Pu isotopic ratios obtained here can be explained by invoking 2-component mixing between remnants of the nuclear fuel used in the Trinity device and that present in the geological background (natural fallout).