Plutonium-244 in the early solar system

Astronomy and Astrophysics – Astrophysics

Scientific paper

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Abundance, Carbonaceous Chondrites, Meteoritic Composition, Planetary Evolution, Plutonium 244, Solar System, Fission, Inclusions, Interstellar Matter, Nuclear Fusion, Petrography, Rare Gases, Xenon

Scientific paper

This paper presents results of noble-gas, fission-track, and petrographic investigations of inclusions in the Allende meteorite, most notably a single large coarse-grained 'high temperature condensate' type inclusion. Discussion of the data focuses on the problem of whether or not Pu-244 actually was present in the early solar system, rather than being represented principally by fission xenon imported into the solar system in interstellar grains. The fission-xenon content of the large inclusion corresponds to a Pu-244/U-238 ratio of about 0.0161 at time of formation, 4.5 billion yr ago. Approximately 30% of this Pu-244 has produced visible fossil fission tracks in the major mineral phases; these decays must have occurred within the solar system, establishing a firm lower limit to the amount of Pu-244 which was present in the solar system. The actual value is almost certainly substantially greater than this lower limit.

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