RAY DIFFRACTION STADY OF STRUCTURE OF CaO—Al2O3—SiO2 TERNARY COMPOUNDS IN MOLTEN AND CRYSTALLINE STATES

  • Vladimir Sokol'skii Taras Shevchenko National University of Kyiv
  • Dmitriy Pruttskov ZAO «Tekhnokhim», Zaporozhye, Ukraine
  • Oleksiy Yakovenko Taras Shevchenko National University of Kyiv
  • Volodymyr Kazimirov Taras Shevchenko National University of Kyiv
  • Oleksandr Roik Taras Shevchenko National University of Kyiv
  • Natalia Golovataya Taras Shevchenko National University of Kyiv
  • Georgii Sokolsky National Technical University of Ukraine "Igor Sikorsky Kyiv Polytechnic Institute

Abstract


Anorthite and gelenite crystalline structure and short range order of anorthite melt have been studied by X-ray diffraction in the temperature range from room temperature to ~1650  C. The corresponding anorthite and gelenite phases were identified as well as amorphous component for anorthite samples having identical shape to XRD pattern of the anorthite melt. The structure factor and the radial distribution function of atoms of the anorthite melt were calculated from the X-ray high-temperature experimental data. The partial structural parameters of the short-range order of the melt were reconstructed using Reverse Monte Carlo simulations.

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Published
2020/09/15
How to Cite
Sokol’skii, V., Pruttskov, D., Yakovenko, O., Kazimirov, V., Roik, O., Golovataya, N., & Sokolsky, G. (2020). RAY DIFFRACTION STADY OF STRUCTURE OF CaO—Al2O3—SiO2 TERNARY COMPOUNDS IN MOLTEN AND CRYSTALLINE STATES. Journal of Mining and Metallurgy, Section B: Metallurgy, 56(2), 269-277. Retrieved from https://aseestant.ceon.rs/index.php/jmm/article/view/23190
Issue
Vol. 56 No. 2 (2020)
Section
Original Scientific Paper

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