Study of the radioactive decay of192Ir

Mehta, D.; Singh, Sukhpal; Garg, M. L.; Singh, Nirmal; Cheema, T.S.; Trehan, P.N.

doi:10.1007/bf01295180

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Ipac-experiments1

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1992

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“…In order to investigate its magnitude and to correct for it we have applied the following procedure: we have analysed very carefully the effect of the superposition of all cascades contributing to the background (including triple and sum peak cascades) using the known values of their relative intensities and anisotropies [4][5][6] and the known ratio COLZ(2+)/COLT(2 +) of the integral rotations in the second and first excited 2 + state [4]. The oversimplifying linear interpolation of the rather large Compton background under the ~468 keV peak produces, of course, a systematic error, but it turned out that this error is quite small.…”

Section: Ipac-experimentsmentioning

confidence: 99%

Measurement of theg-factor of the 21 + state of192Pt in an external magnetic field

Bodenstedt

Hamer

Herzog

et al. 1992

Z. Physik A - Hadrons and Nuclei

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The g-factor of the 2~ state of 192pt has been measured by the IPAC technique in an external magnetic field as: g(2 +, 192pt)= +0.287(17). An additional IPAC experiment with an ~92IrFe sample was performed with the same level in order to investigate the hyperfine field. The result: COLZ(2~-, ~92PtFe)=0.1115(9) gives the hyperfine field: B4?2K(PtFe)= 126-.8(71) T. The result of an LTNO experiment with the same level is compatible with the assumption that 100% of the 192Ir atoms were on unique sites.

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