5840 J. Phys. Chem. B, Vol. 101, No. 30, 1997
Jobic et al.
The mean free distance l between methane molecules can be
et al.24 for a slightly larger molecule (σ ) 5 Å) showing pure
single-file diffusion in AlPO4-5.
derived from the relation41
The explanation we offer for the experimental discrepancies
is that the observation or nonobservation of single-file diffusion
decisively depends on the real structure of the adsorbent under
study. In all these studies, different AlPO4-5 crystals have been
used. It is mentioned in ref 20 that some samples adsorbed 4
molecules/uc, but others 6 molecules/uc. It is also known that
the crystallinity of this material deteriorates with time and water
moisture44 and that the calcination procedure must be slow
enough to avoid defects or partial collapse of the structure.
To explain the discrepancy between our QENS results for
ethane and the MD investigation,24 one may speculate that the
results of MD simulations in this particular structure will be
affected by subtle changes of the potential, as shown in ref 22.
Furthermore, the simulations were performed with a rigid
framework, neglecting the influence of lattice vibrations, which
might have an effect for such a limiting case.
1 - θ
θ
l )
σ
(15)
where σ is the kinetic diameter of the methane molecule.
For a medium concentration, θ ) 0.48, l is equal to 4 Å, and
thus l < λ. In this case, the mutual encounters between adjacent
diffusants become relevant, ensuring the necessary condition
for single-file behavior.
For a small concentration, θ ) 0.11, l is equal to 31 Å, and
thus l > λ. Molecular diffusion is then essentially unaffected
by the other molecules. Depending on the rate of momentum
and energy exchange with the zeolite lattice, molecular propaga-
tion can be described by the ballistic stage or, for sufficiently
fast momentum exchange, by ordinary diffusion.37
It is possible to relate the single-file mobility factor, F, with
a diffusivity that could be measured at infinitely small concen-
tration, Di.41,42 The expression derived by Hahn and co-
workers41 is simply
Conclusion
Two different diffusion regimes have been measured with
the quasi-elastic neutron scattering technique, by varying the
concentration of molecules in 1D channel structures. Ordinary
1D diffusion is observed at low loading for cyclopropane in
AlPO4-5 and for methane in ZSM-48. At higher loadings,
single-file diffusion is found for both systems. The crossover
between the two regimes is attributed to the variation of the
mean free distance between molecules with respect to the space
scale of the present QENS experiments. Ordinary 1D diffusion
is observed for methane and ethane in AlPO4-5, whatever the
loading. It is probable that the different origin of the samples
explains the discrepancies found with PFG NMR results in this
aluminophosphate. Comparative studies with identical sample
materials are thus required. In ZSM-48, the mobility factor of
methane at medium concentration is 2 × 10-12 m2 s-1/2. This
yields a diffusivity for an isolated molecule more than 4 orders
of magnitude larger than the diffusivity derived at low loading,
which seems surprising. It is clear that the characterization of
single-file diffusion is a fairly recent topic and that it deserves
further studies.
F2
Di ) π
(16)
l2
For methane in ZSM-48, at medium concentration, F was
found to be 2 × 10-12 m2 s-1/2. Using eq 16, this gives a value
of 7 × 10-5 m2 s-1 for Di, which would be in striking contrast
to the diffusion coefficient D ) 2.5 × 10-9 m2 s-1, directly
measured for θ ) 0.11. The diffusivity of an isolated molecule
would then be more than 4 orders of magnitude larger than the
diffusivity derived for θ ) 0.11. This discrepancy could be
due to the fact that mutual collisions of the molecules occur
already for θ ) 0.11. Additional measurements are planned,
with a better elastic resolution, to measure single-file diffusion
with a better accuracy.
In the more open 1D channel system of AlPO4-5, best fits
between the experimentally observed scattering behavior and
transport models have been obtained with normal 1D diffusion,
for methane and ethane. It appears that the experimental and
simulation results reported so far in the literature about the
transport properties of the light alkanes in AlPO4-5 are in
disagreement. For methane, the PFG NMR measurements of
Kukla et al. were interpreted by a single-file diffusion model,18
whereas according to another study methane is found to conform
to normal 1D diffusion.19 Quite recently, ordinary 1D diffusion
was found by Martin et al. using QENS.43 The diffusion
coefficient reported by Nivarthi et al. is 2.9 × 10-9 m2 s-1 at
300 K, which is in keeping with our value of 1.6 × 10-9 m2
s-1, at 155 K, for the same concentration of 0.7 molecule/uc.
For larger loadings, the diffusion coefficient derived from the
other QENS experiment43 is 1.0 × 10-9 m2 s-1, at 97 K, for
1.2 molecule/uc, in good agreement with our value of 1.2 ×
10-9 m2 s-1, obtained at 155 K for 1 molecule/uc. We note
that recent MD simulations for methane in this structure24 are
also in favor of ordinary 1D diffusion. However, it is also found
in this work24 that ethane molecules cannot pass each other
easily and exhibit a mobility in between single-file and normal
1D diffusion. Experimentally, the same group has found by
PFG NMR that ethane molecules follow single-file diffusion,42
while our present QENS results suggest ordinary 1D diffusion.
For cyclopropane, we find that this molecule follows single-
file diffusion. This could be the reason for the slow desorption
rates observed during the gravimetric measurements. This
molecule would correspond to the simulation made by Keffer
Acknowledgment. The neutron experiments were performed
at the Institut Laue-Langevin, Grenoble, France. Two of us, K.H.
and J.K., are obliged to the Deutsche Forschungsgemeinschaft
(Sonderforschungbereich 294) for financial support. We also
thank Dr. J. Caro, Institut fu¨r Angewandte Chemie-Berlin, for
discussions.
References and Notes
(1) Ka¨rger, J.; Ruthven, D. M. Diffusion in Zeolites and Other
Microporous Solids; Wiley: New York, 1992.
(2) June, R. L.; Bell, A. T.; Theodorou, D. N. J. Phys. Chem. 1992,
96, 1051.
(3) Maginn, E. J.; Bell, A. T.; Theodorou, D. N. J. Phys. Chem. 1996,
100, 7155.
(4) Meier, W. M., Olson, D. H., Baerlocher, Ch., Eds. Atlas of Zeolites
Structure Types; Elsevier: Amsterdam, Zeolites 17, 1996.
(5) Jobic, H.; Be´e, M.; Kearley, G. J. J. Phys. Chem. 1994, 98, 4660.
(6) Jobic, H.; Be´e, M.; Caro, J.; Bu¨low, M.; Ka¨rger, J.; Pfeifer, H. In
Studies in Surface Science and Catalysis; Ohlmann, G., Pfeifer, H., Fricke,
R., Eds.; Elsevier: Amsterdam, 1991; Vol. 65, p 445.
(7) Jobic, H.; Be´e, M.; Ka¨rger, J.; Pfeifer, H.; Caro, J. J. Chem. Soc.,
Chem. Commun. 1990, 341.
(8) Cohen de Lara, E.; Kahn, R. J. Phys. 1981, 42, 1029.
(9) Kahn, R.; Cohen de Lara, E.; Viennet, E. J. Chem. Phys. 1989, 91,
5097.
(10) Hong, U.; Ka¨rger, J.; Kramer, R.; Pfeifer, H.; Seiffert, G.; Mu¨ller,
U.; Unger, K. K.; Lu¨ck, H. B.; Ito, T. Zeolites 1991, 11, 816.