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. Author manuscript; available in PMC: 2020 Mar 12.
Published in final edited form as: J Radioanal Nucl Chem. 2019;322(3):10.1007/s10967-019-06711-6. doi: 10.1007/s10967-019-06711-6

Table 3.

IDMS sample data and measurement results for the molality of 233Pa in the S solution

Sample ID 233Pa S solution* aliquots (g) U reverse-spike aliquots (g) Measured isotope ratio n(238U)/n(233U) Molality of 233Pa (pmol g−1)
233Pa 1A 2.0640 ± 0.0010 0.3613 ± 0.0010 132.21 ± 0.30 0.14680 ± 0.00057
233Pa 1B 2.0586 ± 0.0010 0.7128 ± 0.0010 261.35 ± 0.59 0.14690 ± 0.00048
233Pa 2A 1.7827 ± 0.0010 0.5993 ± 0.0010 254.01 ± 0.58 0.14676 ± 0.00049
233Pa 2B 2.3084 ± 0.0010 0.6633 ± 0.0010 216.67 ± 0.49 0.14705 ± 0.00049
233Pa 3A 1.6769 ± 0.0010 0.3569 ± 0.0010 160.64 ± 0.37 0.14692 ± 0.00057
233Pa 3B 2.5439 ± 0.0010 0.4086 ± 0.0010 121.31 ± 0.28 0.14683 ± 0.00055
233Pa 4A 1.9842 ± 0.0010 0.6033 ± 0.0010 229.45 ± 0.51 0.14693 ± 0.00049
233Pa 4B 2.2204 ± 0.0010 0.4804 ± 0.0010 163.19 ± 0.37 0.14700 ± 0.00052

The quantity measured by IDMS was the molality of 233U in the decayed S solution (pmol 233U g−1). Corrections for solution evaporation and undecayed 233Pa were applied to the IDMS data to yield molality of 233Pa at the reference time of 27 June 2017 22:50 UTC. Uncertainties are expanded uncertainties (U=kuc) with a coverage factor (k) of 2. All mass values are corrected for air buoyancy

*

Correction factors for 233Pa sample aliquots were applied to compensate for relatively small evaporative losses (from 0.3 to 1.0%) that occurred over the interval between dispensing and aliquoting for IDMS (298 d). These factors were calculated as the quotient of the solution mass at the time of initial dispensing and the solution mass immediately prior to aliquoting for IDMS analyses