E2M1Mixing Ratio of the 123-keV Transition inFe57Determined from a Mössbauer Coincidence Experiment

Abstract
For gamma cascades (2)γ2(1)γ1(0) in nuclei where the separate magnetic components of the ground-state transition (1) → (0) can be observed by the Mössbauer effect because there is a strong internal magnetic field, information about the multipole character of γ2 and γ1 can be obtained by measuring the relative intensities of the magnetic components of γ1 in coincidence with γ2 for specified emission angles of γ1 and γ2 with respect to an external polarizing field. In particular, the mixing ratio of γ2 can be determined if the spins of the levels and the multiple character of γ1 are known. One advantage of this method over normal γγ directional correlation experiments is that the populations of the sublevels of state (1) are independent of the precession of the nuclear spin axis around the field direction. This makes the method especially suitable for cases where the lifetime of state (1) is so long that the directional correlation is appreciably affected by the precession. Another advantage of the method is that there is no averaging effect of the summation over the sublevels. The method has been used to determine the E2M1 mixing ratio of the 123-keV transition in the (52)123 keV(32)14.4 keV(12) cascade in Fe57. Both gamma rays were observed under angles of 90° with respect to the field magnetizing the Armco foil in which the Co57 activity was diffused. Designating the intensities of the components of γ1 observed in coincidence with γ2 by I1cI6c (from low to high energy) the following ratios were measured: I1cI2c=0.91±0.035 and I6cI5c=0.89±0.035. Taking into account incomplete magnetization of the source and finite solid angles of the counters, an E2M1 mixing ratio δ=0.15±0.035 is derived from these ratios.

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