Mean Life of the 1.61-Mev Level ofMg25

Abstract
Nuclear resonance fluorescence techniques have been used to measure the mean life of the 1.61-Mev level of Mg25 and the 1.83-Mev level of Mg26. The exciting γ radiation was obtained by bombarding metallic Mg25 and Mg26 targets with 4.0- and 4.4-Mev protons. For the Mg25 level, assumed to be 72+, the self-absorption of the resonance radiation gives τ=(2.50.4+0.6)×1014 sec. The angular distribution for the resonance scattering was found to be 1+(0.42±0.03)P2(cosθ)+(0.03±0.003)P4(cosθ), where the errors given are statistical only. For other reasons it is believed that the correct coefficient of the P4 term is approximately zero. For the Mg26 level, the apparent resonance scattering cross section combined with some previous estimates of slowing-down times for the excited nuclei gives τ=(7±3)×1013 sec. Further evidence as to the collective nature of these nuclei and of Al27 is discussed. Support is given to the suggestion of the Chalk River group that the 1.61-Mev Mg25 and the 2.21-Mev Al27 levels are the 72+ second members of K=52+ rotational bands based on the ground states. For the Mg25 level, spin and parity 72+ is required to obtain agreement between the quadrupole transition probability from these measurements and that found by Coulomb excitation.