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.

中文翻译：

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Mössbauer探针诊断天然来源的铝硅酸盐表面上的准液体水层的特性

摘要

使用基于⁵⁷ FeMössbauer同位素的两种形式（Fe ²⁺和Fe ³⁺）开发的探针技术，研究了“冻结水粘土矿物”系统中准液态水层的结构和性质。。在分形几何形状内估计表面冰的弹性参数（剪切模量，泊松比和Grüneisen参数）。随着层厚的增加，建立了“ Menger海绵”-“ Cantor灰尘”过渡。