Abstract
Aluminosilicates, differing in their composition and their crystallinity, are labeled with radioactive molybdenum. 99Mo tied to the aluminosilicate network decays to 99mTc. The parameters that determine the separation of 99mTc from 99Mo are studied in crystalline samples (Mo-exchanged Y zeolite) and in amorphous samples (Mo-exchanged collapsed zeolites and Mo-exchanged pumice stone). The efficiency of the separation process is attributed to the environment of molybdenum in the solid.
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