Get 20M+ Full-Text Papers For Less Than $1.50/day. Start a 14-Day Trial for You or Your Team.

Learn More →

Mössbauer Probe Diagnostics of the Properties of Quasi-Liquid Water Layer on the Aluminosilicate Surface of Natural Origin

Mössbauer Probe Diagnostics of the Properties of Quasi-Liquid Water Layer on the Aluminosilicate... The structure and properties of the quasi-liquid water layer in the “frozen water–clay mineral” system have been studied using a probe technique developed on the basis of the 57Fe Mössbauer isotope in two forms (Fe2+ and Fe3+). The elasticity parameters (shear modulus, Poisson’s ratio, and Grüneisen parameter) of the surface ice are estimated within the fractal geometry. The “Menger sponge"–"Cantor dust” transition with an increase in the layer thickness is established. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Crystallography Reports Springer Journals

Mössbauer Probe Diagnostics of the Properties of Quasi-Liquid Water Layer on the Aluminosilicate Surface of Natural Origin

Crystallography Reports , Volume 65 (3) – May 27, 2020

Loading next page...
 
/lp/springer-journals/m-ssbauer-probe-diagnostics-of-the-properties-of-quasi-liquid-water-eh7X34A6DO

References (13)

Publisher
Springer Journals
Copyright
Copyright © Pleiades Publishing, Inc. 2020
ISSN
1063-7745
eISSN
1562-689X
DOI
10.1134/S1063774520030360
Publisher site
See Article on Publisher Site

Abstract

The structure and properties of the quasi-liquid water layer in the “frozen water–clay mineral” system have been studied using a probe technique developed on the basis of the 57Fe Mössbauer isotope in two forms (Fe2+ and Fe3+). The elasticity parameters (shear modulus, Poisson’s ratio, and Grüneisen parameter) of the surface ice are estimated within the fractal geometry. The “Menger sponge"–"Cantor dust” transition with an increase in the layer thickness is established.

Journal

Crystallography ReportsSpringer Journals

Published: May 27, 2020

There are no references for this article.