1991
DOI: 10.1016/s0167-2991(08)61359-2
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Sorption of argon and nitrogen on network types of zeolites and aluminophosphates

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Cited by 23 publications
(10 citation statements)
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“…Such a phenomenon cannot be observed at T = 77.3 K, because of the too-low-pressure value of the substep ( P sub = 4.0 × 10 -2 Torr), which prevents the possibility of measuring the substep desorption branch. In addition, we have to notice that the relative pressure of the substep adsorption branch increases when the temperature increases, P sub / P o = 4.5 10 -2 at T = 96.5 K. The hysteresis loop, related to the sorbed phase transition, has been already found for the system nitrogen/silicalite I …”
Section: Resultsmentioning
confidence: 68%
“…Such a phenomenon cannot be observed at T = 77.3 K, because of the too-low-pressure value of the substep ( P sub = 4.0 × 10 -2 Torr), which prevents the possibility of measuring the substep desorption branch. In addition, we have to notice that the relative pressure of the substep adsorption branch increases when the temperature increases, P sub / P o = 4.5 10 -2 at T = 96.5 K. The hysteresis loop, related to the sorbed phase transition, has been already found for the system nitrogen/silicalite I …”
Section: Resultsmentioning
confidence: 68%
“…But this does not necessarily mean that the distribution of different sorption centers between crystallographically determined sites, such as segments of 1 a" « 0.45 mmol/cm3 u" = 1.81 mmol/cm3 0.0091 1/Pa 0.14 1/Pa sinusoidal and straight channels, obeys that factor. In this respect, recent findings of sorption state transitions between "disordered phases" and "crystalline-like solid phases" for various gases in MFI,33 34 expressed also as isotherm hysteresis at low temperature and loading, are of interest. To correlate the above probability of distribution to any identified number of sorption centres or types of sorption states may well be a task of further studies.…”
Section: Resultsmentioning
confidence: 99%
“…As a matter of fact this time for N 2 in NaA is very long at 193 K; it is then difficult to perform isotherms at lower temperatures because of the temperature regulation. At 78 K, the diffusivity of N 2 in NaA is completely hindered, meanwhile O 2 continues to diffuse easily in this zeolite; the Na cations in the window aperture impede totally the intracrystalline diffusion of N 2 . This fact has been used to verify the quantity which can be condensed in the intergrain volume.…”
Section: Methodsmentioning
confidence: 99%