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. Author manuscript; available in PMC: 2022 Apr 1.
Published in final edited form as: Appl Radiat Isot. 2020 Dec 31;170:109572. doi: 10.1016/j.apradiso.2020.109572

Table 2.

Sources measured at NIST for this study. Activities (A) for the sources prepared at NIST were determined by triple-to-double coincidence ratio (TDCR) counting. All times are UTC.

Source ID t sep t ref A/Bq Technique
E2-A1 2018–09-14 18:15 2018–09-27 17:00 1.3121(30) × 106 TDCR
E2-A2 2018–09-14 18:15 2018–09-27 17:00 1.2773(29) × 106 TDCR
E2-D1- A1 2018–09-14 18:15 2018–09-27 17:00 1.2465(28) × 106 TDCR
E3-A2 2018–10-31 17:00a 2018–11-06 17:00 1.603(7) × 106 TDCR
E4-A2 2019–02-08 20:40 2019–02-15 17:00 6.073(15) × 106 TDCR
S3-A 2019–12-04 10:56 2019–12-13 12:00 1.503(8) × 105b VIC
a

The separation time for the E3 source was not communicated by ORNL, but was estimated based on the shipping schedule and observed equilibrium.

b

The comparison ampoule contained 5.01700 g of solution S3 (see Table 1). The activity given here was measured at NIST using the Vinten 671 ionization chamber (VIC).