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Adsorption of Ar into zeolite Al-MFI (NH4)

Published online by Cambridge University Press:  08 February 2024

Colin W. Scherry
Affiliation:
North Central College, 131 S. Loomis St., Naperville, IL 60540, USA
James A. Kaduk*
Affiliation:
North Central College, 131 S. Loomis St., Naperville, IL 60540, USA Illinois Institute of Technology, 3101 S. Dearborn St., Chicago, IL 60616, USA
Winnie Wong-Ng
Affiliation:
Materials Measurement Science Division, National Institute of Standards and Technology, Gaithersburg, MD 20899-8520, USA
Huong Giang T. Nguyen
Affiliation:
Chemical Sciences Division, National Institute of Standards and Technology, Gaithersburg, MD, 20899-8390, USA
*
a)Author to whom correspondence should be addressed. Electronic mail: kaduk@polycrystallography.com

Abstract

The crystal structure of anhydrous Al-MFI (NH4) containing adsorbed Ar has been determined and refined using synchrotron X-ray powder diffraction data taken at 90 K, and optimized using density functional theory techniques. Six highly occupied Ar sites almost completely fill the pore volume of the zeolite. Changing the gas flow from Ar to He at 90 K decreases the Ar occupancies of all six sites, but two decrease more than the others. Warming the sample from 90 to 295 K in Ar flow results in further decreases in site occupancies, but five of the original six sites persist.

Information

Type
Technical Article
Copyright
Copyright © The Author(s), 2024. Published by Cambridge University Press on behalf of International Centre for Diffraction Data
Figure 0

Figure 1. The crystal structure of zeolite MFI as viewed down the orthorhombic c-axis. Si atoms are colored tan, and O atoms are red. The yellow surface indicates the pores, with a probe radius of 1.2 Å. The straight channels (vertical) lie parallel to the b-axis, and the zig-zag channels (horizontal) join them along the a-axis. Image generated using Mercury (Macrae et al., 2020).

Figure 1

TABLE I. Refinement residuals for Ar-MFI study.

Figure 2

Figure 2. The Rietveld plot for the refinement of Al-MFI (Ar), using dataset 11bmb_8192. The blue crosses represent the observed data points, and the green line is the calculated pattern. The cyan curve is the normalized error plot, and the red line is the background curve. The vertical scale has been multiplied by a factor of 10× for 2θ > 10.0°, and by a factor of 40× for 2θ > 22.0°.

Figure 3

Figure 3. Changes in a small portion of the X-ray powder diffraction pattern of MFI as a function of temperature and atmosphere. Image generated using JADE Pro (MDI, 2023).

Figure 4

Figure 4. The crystal structure of Al-MFI (NH4) is viewed down the b-axis. The straight channels are parallel to the b-axis, and the zig-zag channels are parallel to the a-axis. Image generated using Diamond (Crystal Impact, 2022).

Figure 5

Figure 5. Changes in the unit cell volume of MFI as a function of temperature and atmosphere.

Figure 6

Figure 6. The crystal structure of Ar-filled MFI is viewed down the b-axis. Ar43 is colored blue, and Ar40 is in purple. The other Ar sites are colored cyan. Image generated using Diamond (Crystal Impact, 2022).

Figure 7

Figure 7. The crystal structure of Ar-filled MFI is viewed down the c-axis. Ar43 is colored blue, and Ar40 is in purple. The other Ar sites are colored cyan. Image generated using Diamond (Crystal Impact, 2022).

Figure 8

TABLE II. Shortest Ar–Ar and Ar–O distances (Å) in Ar-MFI at 90 K (run 11bmb_8192).

Figure 9

Figure 8. Ar site occupancies (uncertainty expressed as standard deviation) at 90 K in MFI as a function of time. The zero of time is the change from Ar to He atmosphere.

Figure 10

TABLE III. Occupancy of Ar sites in MFI at different temperatures and gas compositions. Standard uncertainty = 0.01 for all values.

Figure 11

TABLE IV. Absolute position differences (Å) for the Ar sites in the VASP-optimized fully occupied structure compared to the optimized structures with individual sites fully occupied.