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Dehydration-induced water disordering in a synthetic potassium gallosilicate natrolite
被引:4
|作者:
Lee, Yongjae
[1
]
Kim, Sun Jin
Bull, Ivor
Celestian, Aaron J.
Parise, John B.
Kao, Chi-Chang
Vogt, Thomas
机构:
[1] Yonsei Univ, Dept Earth Syst Sci, Seoul 120749, South Korea
[2] Korea Inst Sci & Technol, Nanomat Res Ctr, Seoul 136791, South Korea
[3] BASF CATALYSTS LLC, Iselin, NJ 08830 USA
[4] Western Kentucky Univ, Dept Geog & Geol, Bowling Green, KY 42101 USA
[5] SUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USA
[6] Brookhaven Natl Lab, Natl Synchrotron Light Source, Upton, NY 11973 USA
[7] Univ S Carolina, NanoCtr, Columbia, SC 29208 USA
[8] Univ S Carolina, Dept Chem & Biochem, Columbia, SC 29208 USA
关键词:
D O I:
10.1021/ja075037z
中图分类号:
O6 [化学];
学科分类号:
0703 ;
摘要:
A new potassium gallosilicate zeolite with a natrolite topology (approximate formula K8.2Ga8.2-Si11.8O40 center dot 11.5H(2)O) was synthesized under hydrothermal conditions and characterized as a function of temperature using monochromatic synchrotron X-ray powder diffraction and Rietveld analyses. Unlike the previously known tetragonal K8Ga8Si12O40 center dot 6H(2)O phase, the as-synthesized material contains twice the amount of water molecules in an ordered arrangement throughout the channels in an orthorhombic (/2(1)2(1)2(1)) symmetry. The ordered configuration of water molecules is stabilized below 300 K, whereas heating above 300 K results in a selective dehydration and subsequent disordering of water molecules in a tetragonal (/42d) symmetry. Above 400 K, the material transforms to a fully dehydrated tetragonal phase with a concomitant volume reduction of ca. 15%. The fully dehydrated material transforms back to its original state when rehydrated over a period of up to 2 weeks. The distribution of potassium cations within the channels remains largely unperturbed during the water rearrangements and their order-disorder transition within the channels.
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页码:13744 / 13748
页数:5
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