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 Mossbauer isotope in two forms (Fe2+ and Fe3+). The elasticity parameters (shear modulus, Poisson’s ratio, and Gruneisen 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.
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