In-situ dehydration studies of fully K-,Rb-, and Cs-exchanged natrolites
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SCOPUS
- Title
- In-situ dehydration studies of fully K-,Rb-, and Cs-exchanged natrolites
- Authors
- Lee, Y; Seoung, DH; Liu, D; Park, MB; Hong, SB; Chen, HY; Bai, JM; Kao, CC; Vogt, T; Lee, Y
- Date Issued
- 2011-02
- Publisher
- MINERALOGICAL SOC AMER
- Abstract
- In-situ synchrotron X-ray powder diffraction studies of K-, Rb-, and Cs-exchanged natrolites between room temperature and 425 degrees C revealed that the dehydrated phases with collapsed frameworks start to form at 175, 150, and 100 degrees C, respectively. The degree of the framework collapse indicated by the unit-cell volume contraction depends on the size of the non-framework cation: K-exchanged natrolite undergoes an 18.8% unit-cell volume contraction when dehydrated at 175 degrees C, whereas Rb- and Cs-exchanged natrolites show unit-cell volume contractions of 18.5 and 15.2% at 150 and 100 degrees C, respectively. In the hydrated phases, the dehydration-induced unit-cell volume reduction diminishes as the cation size increases and reveals increasingly a negative slope as smaller cations are substituted into the pores of the natrolite structure. The thermal expansion of the unit-cell volumes of the dehydrated K-, Rb-, and Cs-phases have positive thermal expansion coefficients of 8.80 x 10(-5) K-1, 1.03 x 10(-4) K-1, and 5.06 x 10-5 K-1, respectively. Rietveld structure refinements of the dehydrated phases at 400 degrees C reveal that the framework collapses are due to an increase of the chain rotation angles, psi, which narrow the channels to a more elliptical shape. Compared to their respective hydrated structures at ambient conditions, the dehydrated K-exchanged natrolite at 400 degrees C shows a 2.2-fold increase in psi, whereas the dehydrated Rb- and Cs-natrolites at 400 degrees C reveal increases of psi by ca. 3.7 and 7.3 tiles, respectively. The elliptical channel openings of the dehydrated K-, Rb-, to Cs-phases become larger as the cation size increases. The disordered non-framework cations in the hydrated K-, Rb-, and Cs-natrolite order during dehydration and the subsequent framework collapse. The dehydrated phases of Rb- and Cs-natrolite can be stabilized at ambient conditions.
- Keywords
- K-; Rb-; Cs-natrolite; dehydration; Rietveld refinement; REFINEMENT; ZEOLITES
- URI
- https://oasis.postech.ac.kr/handle/2014.oak/25036
- DOI
- 10.2138/AM.2011.3678
- ISSN
- 0003-004X
- Article Type
- Article
- Citation
- AMERICAN MINERALOGIST, vol. 96, no. 2-3, page. 393 - 401, 2011-02
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- There are no files associated with this item.
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