Transformation of the Surface Structure of Marble under the Action of a Shock Wave

I. P. Shcherbakov; V. I. Vettegren; A. Ya. Bashkarev; R. I. Mamalimov

doi:10.1134/S106378421801022X

Transformation of the Surface Structure of Marble under the Action of a Shock Wave

作者: Shcherbakov I.P.¹, Vettegren V.I.¹, Bashkarev A.Y.², Mamalimov R.I.¹
隶属关系:
1. Ioffe Institute
2. Peter the Great St. Petersburg Polytechnic University
期: 卷 63, 编号 1 (2018)
页面: 78-82
栏目: Physics of Nanostructures
URL: https://ogarev-online.ru/1063-7842/article/view/200533
DOI: https://doi.org/10.1134/S106378421801022X
ID: 200533

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The structure of marble fracture fragments formed after the destruction under the action of a shock wave have been analyzed by Raman, infrared, and luminescence spectroscopic techniques. It has been found that calcite I in the surface layer of fragments with thicknesses of about 2 μm is transformed into high-pressure phase calcite III. At the same time, concentrations of Mn²⁺, Eu³⁺, and other ions decrease to about onefourth of their initial values.