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Ag-exchanged analcime: crystal structure and crystal chemistry
The crystal structure of Ag-substituted analcime (Ag 1.88[Al 1.88Si 4.12O 12]·2H 2O) prepared by ion exchange of Ag + for Na + was studied by single-crystal X-ray diffraction. The monoclinic unit cell parameters are a=19.369(3) Å, b=13.752(2) Å, c=19.385(2) Å, γ=90.26(1)°, V=5163(1) Å 3, Z=16, space...
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Published in: | Microporous and mesoporous materials 2000-09, Vol.39 (1), p.265-273 |
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Main Authors: | , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | The crystal structure of Ag-substituted analcime (Ag
1.88[Al
1.88Si
4.12O
12]·2H
2O) prepared by ion exchange of Ag
+ for Na
+ was studied by single-crystal X-ray diffraction. The monoclinic unit cell parameters are
a=19.369(3) Å,
b=13.752(2) Å,
c=19.385(2) Å,
γ=90.26(1)°,
V=5163(1) Å
3,
Z=16, space group:
F112/
d (No. 15). A comparison was made with the structure of the original Na-analcime. The Ag
+ cations are located in the vicinity of the former Na positions and octahedrally coordinated (O
4(H
2O)
2). The larger Ag
+ cations enter the rectangular O
4-windows relatively easily. Only the Ag–OH
2 distances increase significantly. The correlation between the population of extra-framework positions and the Si/Al distribution is significantly better in the Ag-analcime than in the initial Na-analcime. Changes in the unit cell parameters and the symmetry are explained from crystal chemical considerations. |
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ISSN: | 1387-1811 1873-3093 |
DOI: | 10.1016/S1387-1811(00)00202-X |