Measurements of the ruthenium isotopic
composition of nuclear samples
could provide information about the method of sample production, sample
irradiation history, and age. To investigate the feasibility and applicability
of this idea, this study focuses on measurements of the ruthenium
isotope composition of a nominally single-isotope 106Ru
radioactivity standard, where the complications of environmental mixing
are eliminated. The measurements of the 106Ru standards
reveal unusual stable ruthenium isotopic compositions consistent with
fissiogenic ruthenium. Three different lots of the material have been
investigated, and the isotopic composition is found to be different
for lot 1 as compared to lots 2 and 3, indicating a longer irradiation
duration incurred during the production of lot 1. Through measurements
of 106Ru and its 106Pd daughter, radiochronometry
can be used to infer the ages of the samples. Lot 1 is older than
lots 2 and 3 and was produced 4.91(5) years before the reference date
of 1/1/21, approximately 2.7 years before lots 2 and 3. In an effort
to better understand the sample production pathway, the isotopic measurements
are compared with nuclear reactor simulations, which suggest that
the material was generated by irradiation of a low-enriched uranium
target material in a light water reactor. These findings have significant
implications for nuclear treaty monitoring, providing an example of
the power of ruthenium isotope measurements to discern details of
sample origin and history.