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This article is cited in 1 scientific paper (total in 1 paper)
Thermophysical Properties of Materials
Rankinite synthesis and pyrolysis inversion
V. S. Engel'shta, V. Zh. Muratalievab a Institute of Physical-Technical Problems and Material Sciences, NAS of Kirgiz Republic, Bishkek
b Kyrgyz State Technical University named after Iskhak Razzakov
Abstract:
The thermal transformation of the pyrolysis–condensation–rankinite synthesis process at a normal pressure is considered in detail. Rankinite pyrolysis is performed with a step-by-step increase in enthalpy (TERRA software system). Rankinite pyrolysis compounds are condensed on a surface with temperature $T = 298.15$ K. Condensate compounds are equivalent to pyrolysis compounds. Wollastonite and limestone can precipitate upon condensation to form a mineral deposit. Synthesis is performed by mixing the condensate compounds. The compounds and heat of chemical reactions, the enthalpy, the temperature, and the heat content have been determined. It has been shown that the decomposition of rankinite $(T_{\rm dec} = 2598.36$ K$)$, wollastonite $(T_{\rm dec} = 3662.7$ K$)$, and limestone $(T_{\rm dec} = 3680$–$3810$ K$)$ occurs in the process of synthesis and pyrolysis at a constant temperature. The complete pyrolysis–condensation–synthesis process picture typical for various compounds is given.
Received: 05.07.2015 Accepted: 22.12.2015
Citation:
V. S. Engel'sht, V. Zh. Muratalieva, “Rankinite synthesis and pyrolysis inversion”, TVT, 55:2 (2017), 233–239; High Temperature, 55:2 (2017), 226–232
Linking options:
https://www.mathnet.ru/eng/tvt4949 https://www.mathnet.ru/eng/tvt/v55/i2/p233
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Abstract page: | 205 | Full-text PDF : | 94 | References: | 38 | First page: | 1 |
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