Abstract
The K-shell internal conversion coefficients of gamma rays from Te123, Sm153, Hf181, and Os191 have been measured using a coincidence scintillation spectrometer employing NaI and anthracene phosphors as detectors. In several cases an unambiguous classification of the transition as to multipole order and character is possible. The results indicate that the 159-kev gamma ray from Te123 is predominantly M1, the 70-kev gamma ray from Sm153 is a mixture of E2+M1, the 132-kev gamma ray from Hf181 is predominantly E2, the 135-kev gamma ray from Hf181 is predominantly M1, the 345-kev and 480-kev gamma rays from Hf181 are a mixture of either E2+M1 or E1+M2, and the 129-kev gamma ray from Os191 is a mixture of either E2+M1 or E1+M2.