Transient hyperfine field measurements of gyromagnetic ratios in Os and Pt nuclei

A. E. Stuchbery, C. G. Ryan, H. Ohnuma, G. B. Beard, and H. H. Bolotin
Phys. Rev. C 27, 434 – Published 1 January 1983
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Abstract

Precessions were measured of the 21+ states in Os192 and Pt198 in the enhanced transient field in thin cobalt foils and comparison made with similar recent studies of Os188 and Pt194 ions in Fe foils. It is concluded that (i) the transient field acting on Pt in Fe is singularly anomalous, and (ii) recent contention by Levy et al. that the g factors of even Pt 21+ states may be substantially lower than reported earlier cannot be sustained.

NUCLEAR REACTIONS Os192(S32, S32′) Os192(21+), Os192(Ni58, Ni58′)- Os192(21+), Pt198(S32, S32′) Pt198(21+), Pt198(Ni58, Ni58′) Pt198(21+), ES=80 MeV, ENi=220 MeV, enriched targets; measured W(θ, H, T) in thin polarized Co. Deduced relative transient field strengths OsCo and PtCo, OsFe and PtFe for 1.5%<~vc<~3.9%, deduced g(21+) even Pt isotopes.

  • Received 31 August 1982

DOI:https://doi.org/10.1103/PhysRevC.27.434

©1983 American Physical Society

Authors & Affiliations

A. E. Stuchbery

  • School of Physics, University of Melbourne, Parkville, Victoria, 3052 Australia and Department of Nuclear Physics, Research School of Physical Sciences, Australian National University, Canberra, A.C.T., 2600 Australia

C. G. Ryan, H. Ohnuma*, G. B. Beard, and H. H. Bolotin

  • School of Physics, University of Melbourne, Parkville, Victoria, 3052 Australia

  • *Permanent address: Department of Physics, Tokyo Institute of Technology, Oh-Okayama, Meguro, Tokyo, Japan.
  • On leave from Department of Physics, Wayne State University, Detroit, Mich.

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Vol. 27, Iss. 1 — January 1983

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