Structural environment of krypton dissolved in vitreous silica

21Citations
Citations of this article
12Readers
Mendeley users who have this article in their library.

Abstract

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 ± 0.1 Å, based on a simple model of Gaussian disorder, with a Debye-Waller factor of σ2 = 0.06 Å2. 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.

Cite

CITATION STYLE

APA

Wulf, R., Calas, G., Ramos, A., Büttner, H., Roselieb, K., & Rosenhauer, M. (1999). Structural environment of krypton dissolved in vitreous silica. American Mineralogist, 84(9), 1461–1463. https://doi.org/10.2138/am-1999-0927

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free