2005
DOI: 10.12693/aphyspola.107.729
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Positronium Trapping in Porous Solids: Means and Limitations for Structural Studies

Abstract: Positron annihilation techniques are used for the structural investigation of solids but the interpretation of results in grainy and porous media is still unclear. A unique picture can be obtained assuming that the dominant process is Ps trapping in competing "extended free volume" sites. In samples with a large amount of free volumes near-saturation Ps trapping will rule the lifetime pattern, and very long lifetimes of over 100 ns might arise from o-Ps trapped in mesopores. It is shown that lifetime parameter… Show more

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Cited by 12 publications
(13 citation statements)
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“…It has been also shown already that even a higher number of lifetime components could be significantly resolved: for silicalite-1 MFI samples five components were extracted. Furthermore, in case of LT measurements performed on the MFI samples in closed N 2 gas atmosphere, at low temperatures due to the capillary condensation into the channels and cages of the zeolite skeleton a newer component-ascribed to a Ps-bubble-like state in the condensed gas-became evident (Kajcsos et al, , 2005, as will be discussed further.…”
Section: Resultsmentioning
confidence: 93%
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“…It has been also shown already that even a higher number of lifetime components could be significantly resolved: for silicalite-1 MFI samples five components were extracted. Furthermore, in case of LT measurements performed on the MFI samples in closed N 2 gas atmosphere, at low temperatures due to the capillary condensation into the channels and cages of the zeolite skeleton a newer component-ascribed to a Ps-bubble-like state in the condensed gas-became evident (Kajcsos et al, , 2005, as will be discussed further.…”
Section: Resultsmentioning
confidence: 93%
“…A satisfactory fit of the LT spectra usually requires at least four lifetime components: 0.2-0.5 ns combining the p-Ps and e + -annihilations, 1-4 ns for o-Ps probably trapped in microvoids of the lattice, 10-90 ns for o-Ps decaying in internal channels of the zeolites and 100-135 ns for o-Ps decaying outside of the crystallites, in the intergrain space , whereas mesopores may also contribute to this latter two components (Kajcsos et al, 2005). It has been also shown already that even a higher number of lifetime components could be significantly resolved: for silicalite-1 MFI samples five components were extracted.…”
Section: Resultsmentioning
confidence: 99%
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