Positron annihilation lifetime spectra of MCM-41 and zeolite Y were measure
d at different vacuum levels. When the experiments were carried out in air,
a very long lifetime component (tau (4) = 35-45 ns, I-4 = 15-20%) was obse
rved for MCM-41, while the longest lifetime for zeolite Y was only 2-4 ns w
ith an intensity of 15-25%. However, when the experiments were carried out
in vacuum, the very long lifetime components could be observed for both sam
ples, although with different intensities, similar to 30% for MCM-41 and si
milar to 10% for zeolite Y. For MCM-41 in air, the longest lifetime (tau (4
)) is similar to 42 ns, corresponding to the ortho-positronium (o-Ps) annih
ilation lifetime in MCM-41 cavities. This value is slightly longer but very
close to the value of 39 ns, which was estimated by using a bouncing quant
um particle model. These peculiar positron annihilation characteristics wer
e explained by air quenching mechanism of o-Ps annihilation in MCM-41. It w
as suggested that because of the existence of the very long lifetime compon
ent even in air, positron lifetime spectroscopy could be a very useful tool
for nondestructive measurement of the cavity size of mesoporous solids suc
h as MCM-41.