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Supercritical Water as Nanomedium for Gasification of Lignite-Water Suspension

The gasification of an aqueous suspension of lignite from Alexandria coalfield (Ukraine) under the supercritical pressure was studied. The initial rates of the formation of hydrogen, carbon dioxide and methane were evaluated. The mutually stimulating interaction of the components of “brown coal-wate...

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Autores principales: Korzh, Raisa, Bortyshevskyi, Valerii
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer US 2016
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4870517/
https://www.ncbi.nlm.nih.gov/pubmed/27194442
http://dx.doi.org/10.1186/s11671-016-1458-x
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author Korzh, Raisa
Bortyshevskyi, Valerii
author_facet Korzh, Raisa
Bortyshevskyi, Valerii
author_sort Korzh, Raisa
collection PubMed
description The gasification of an aqueous suspension of lignite from Alexandria coalfield (Ukraine) under the supercritical pressure was studied. The initial rates of the formation of hydrogen, carbon dioxide and methane were evaluated. The mutually stimulating interaction of the components of “brown coal-water-mineral matter” system was shown due to the influence of nanoscaled water medium on the formation of dipole-inductive, dispersive and ionic associates. In the temperature range of 300–450 °C, the oxygen source for gaseous products of the lignite supercritical gasification is mainly ion-associative nanoclustered water. The source of hydrogen at the subcritical temperature is the organic part of brown coal. For the supercritical water, the source of H is the nanoscale medium with ion associates. The last ones were responsible for the further transformation of coal.
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spelling pubmed-48705172016-06-21 Supercritical Water as Nanomedium for Gasification of Lignite-Water Suspension Korzh, Raisa Bortyshevskyi, Valerii Nanoscale Res Lett Nano Express The gasification of an aqueous suspension of lignite from Alexandria coalfield (Ukraine) under the supercritical pressure was studied. The initial rates of the formation of hydrogen, carbon dioxide and methane were evaluated. The mutually stimulating interaction of the components of “brown coal-water-mineral matter” system was shown due to the influence of nanoscaled water medium on the formation of dipole-inductive, dispersive and ionic associates. In the temperature range of 300–450 °C, the oxygen source for gaseous products of the lignite supercritical gasification is mainly ion-associative nanoclustered water. The source of hydrogen at the subcritical temperature is the organic part of brown coal. For the supercritical water, the source of H is the nanoscale medium with ion associates. The last ones were responsible for the further transformation of coal. Springer US 2016-05-18 /pmc/articles/PMC4870517/ /pubmed/27194442 http://dx.doi.org/10.1186/s11671-016-1458-x Text en © Korzh and Bortyshevskyi. 2016 Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made.
spellingShingle Nano Express
Korzh, Raisa
Bortyshevskyi, Valerii
Supercritical Water as Nanomedium for Gasification of Lignite-Water Suspension
title Supercritical Water as Nanomedium for Gasification of Lignite-Water Suspension
title_full Supercritical Water as Nanomedium for Gasification of Lignite-Water Suspension
title_fullStr Supercritical Water as Nanomedium for Gasification of Lignite-Water Suspension
title_full_unstemmed Supercritical Water as Nanomedium for Gasification of Lignite-Water Suspension
title_short Supercritical Water as Nanomedium for Gasification of Lignite-Water Suspension
title_sort supercritical water as nanomedium for gasification of lignite-water suspension
topic Nano Express
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4870517/
https://www.ncbi.nlm.nih.gov/pubmed/27194442
http://dx.doi.org/10.1186/s11671-016-1458-x
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