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American Mineralogist; September 1999; v. 84; no. 9; p. 1461-1463
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Structural environment of krypton dissolved in vitreous silica

Reinhard Wulf, George Calas, Aline Ramos, Heinz Buettner, Knut Roselieb, and Matthias Rosenhauer

Mineralogische-Petrologisches Institut der Universitaet Goettingen, Gottingen, Federal Republic of Germany

X-ray absorption measurements on Kr dissolved homogeneously in vitreous silica (1.97 wt% Kr) have been carried out at the Kr K-edge at 4.5 K, representing the first direct determination of the sites occupied by a noble gas. The presence of EXAFS oscillations shows that the Kr atoms are surrounded by a well-defined shell of nearest neighbors, identified as oxygen atoms. The mean Kr-O distances are 3.45+ or -0.1 Aa, based on a simple model of Gaussian disorder, with a Debye-Waller factor of sigma 2 = 0.06 Aa 2 . The large Kr-O distance, which is at the upper limit of the size of the holes existing in vitreous silica, together with the existence of well-defined sites suggests a forced, densely packed environment of oxygen around Kr atoms characteristic of clathrasil surroundings.

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L. Zhang, J. A. Van Orman, and D. J. Lacks
Effective radii of noble gas atoms in silicates from first-principles molecular simulation
American Mineralogist, April 1, 2009; 94(4): 600 - 608.
[Abstract] [Full Text] [PDF]




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