Email this article Combustion of carbonized coal residue in water–oxygen supercritical fluid
- Authors: Vostrikov A.A.1, Fedyaeva O.N.1, Dubov D.Y.1, Shishkin A.V.1, Sokol M.Y.1
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Affiliations:
- Kutateladze Institute of Thermal Physics, Siberian Branch
- Issue: Vol 52, No 5 (2016)
- Pages: 562-565
- Section: Article
- URL: https://ogarev-online.ru/0010-5082/article/view/152603
- DOI: https://doi.org/10.1134/S0010508216050075
- ID: 152603
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Abstract
The autothermal regime of partial oxidation of carbonized coal residue in a stream of water-oxygen fluid at 923 K and 30 MPa is implemented for the first time. It is revealed that the oxidation of coal residue and the formation of combustible gases (hydrogen content in the products is increased by 26% with respect to its amount in the original sample) occur simultaneously and are caused by the participation of the H2O molecules in the redox reactions.
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About the authors
A. A. Vostrikov
Kutateladze Institute of Thermal Physics, Siberian Branch
Author for correspondence.
Email: vostrikov@itp.nsc.ru
Russian Federation, Novosibirsk, 630090
O. N. Fedyaeva
Kutateladze Institute of Thermal Physics, Siberian Branch
Email: vostrikov@itp.nsc.ru
Russian Federation, Novosibirsk, 630090
D. Yu. Dubov
Kutateladze Institute of Thermal Physics, Siberian Branch
Email: vostrikov@itp.nsc.ru
Russian Federation, Novosibirsk, 630090
A. V. Shishkin
Kutateladze Institute of Thermal Physics, Siberian Branch
Email: vostrikov@itp.nsc.ru
Russian Federation, Novosibirsk, 630090
M. Ya. Sokol
Kutateladze Institute of Thermal Physics, Siberian Branch
Email: vostrikov@itp.nsc.ru
Russian Federation, Novosibirsk, 630090
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