Decay of Y85 Isomers

I. Dostrovsky, S. Katcoff, and R. W. Stoenner
Phys. Rev. 132, 2600 – Published 15 December 1963
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Abstract

Two isomers of Y85 have been identified and their half-lives determined as 2.68±0.05 h and 5.0±0.2 h. Measurements were made by means of successive timed daughter separations and by direct observation of the decay of radiations from yttrium. Both isomers decay independently by positron emission. The 2.68-h isomer decays to the 70-min Sr85m while the 5.0-h isomer decays to the 64-d Sr85. No isomeric transition was observed. Positron spectra were measured with a β-ray spectrometer. The spectrum for the 2.68-h isomer has an end-point energy of 1.54±0.02 MeV, and the components of the 5-h isomer have end points of 2.24±0.01 MeV, 2.01±0.01 MeV, and 1.1±0.1 MeV. Conversion electron measurements disclosed a 503-keV transition, with a half-life of 2.68 h, K conversion coefficient of 1.9×103, and KL ratio of ∼10. The γ spectrum for the Y85 isomeric mixture is complex. The observed transitions are: 503 and 925 keV from the 2.68-h isomer, and 231, 700, 772, (1030), (1130), 1230, 1390, 1590, 1870, 2160, 2340, and 2750 keV from the 5.0-h isomer. Sum-coincidence spectra showed summation of the following radiations: (231-511), (503-511), (231-1390), and (772-1390) keV. Beta-gamma coincidence measurements showed that the 2.01-MeV positron group is coincident with the 231-keV γ ray and that the 1.54-MeV positron from the 2.68-h isomer is in coincidence with the 503-keV γ ray. The 5.0-h isomer of Y85 is 3.26 MeV above the ground level of Sr85 while the 2.68-h isomer is at 3.30 MeV, thus being 40±30 keV higher. Spins of 92+ and ½- have been assigned to the 5.0-h and 2.68-h isomers, respectively. A partial decay scheme is presented.

  • Received 22 July 1963

DOI:https://doi.org/10.1103/PhysRev.132.2600

©1963 American Physical Society

Authors & Affiliations

I. Dostrovsky*, S. Katcoff, and R. W. Stoenner

  • Chemistry Department, Brookhaven National Laboratory, Upton, New York

  • *On leave of absence from the Weizmann Institute of Science, Rehovoth, Israel.

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Vol. 132, Iss. 6 — December 1963

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