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Thermal behaviour of romarchite phase SnO in different atmospheres: a hypothesis about the phase transformation

A study was conducted on the transformation of SnO to SnO(2) using X-ray diffraction and subjecting the SnO to heat treatments between 300 °C < T < 600 °C in two different atmospheres, argon and air. The intermediary oxide that appears in the disproportionation process was identified as Sn(2)O...

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Detalles Bibliográficos
Autores principales: Campo, Carlos M., Rodríguez, Jorge E., Ramírez, Alfonso E.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Elsevier 2016
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4946215/
https://www.ncbi.nlm.nih.gov/pubmed/27441283
http://dx.doi.org/10.1016/j.heliyon.2016.e00112
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author Campo, Carlos M.
Rodríguez, Jorge E.
Ramírez, Alfonso E.
author_facet Campo, Carlos M.
Rodríguez, Jorge E.
Ramírez, Alfonso E.
author_sort Campo, Carlos M.
collection PubMed
description A study was conducted on the transformation of SnO to SnO(2) using X-ray diffraction and subjecting the SnO to heat treatments between 300 °C < T < 600 °C in two different atmospheres, argon and air. The intermediary oxide that appears in the disproportionation process was identified as Sn(2)O(3). In an argon atmosphere, decomposition occurs in three stages: (1) a direct transformation of SnO to SnO(2), (2) the formation of some intermediary Sn(2)O(3) from SnO, and (3) the conversion of the Sn(2)O(3) to SnO(2) with the formation of metallic tin, Sn (l). When an atmosphere of air is used, however, a reaction occurs, concurrent with the decomposition reactions, that relates to the specific oxidation of the metallic tin produced in the course of the three process stages.
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spelling pubmed-49462152016-07-20 Thermal behaviour of romarchite phase SnO in different atmospheres: a hypothesis about the phase transformation Campo, Carlos M. Rodríguez, Jorge E. Ramírez, Alfonso E. Heliyon Article A study was conducted on the transformation of SnO to SnO(2) using X-ray diffraction and subjecting the SnO to heat treatments between 300 °C < T < 600 °C in two different atmospheres, argon and air. The intermediary oxide that appears in the disproportionation process was identified as Sn(2)O(3). In an argon atmosphere, decomposition occurs in three stages: (1) a direct transformation of SnO to SnO(2), (2) the formation of some intermediary Sn(2)O(3) from SnO, and (3) the conversion of the Sn(2)O(3) to SnO(2) with the formation of metallic tin, Sn (l). When an atmosphere of air is used, however, a reaction occurs, concurrent with the decomposition reactions, that relates to the specific oxidation of the metallic tin produced in the course of the three process stages. Elsevier 2016-05-11 /pmc/articles/PMC4946215/ /pubmed/27441283 http://dx.doi.org/10.1016/j.heliyon.2016.e00112 Text en © 2016 The Authors http://creativecommons.org/licenses/by-nc-nd/4.0/ This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
spellingShingle Article
Campo, Carlos M.
Rodríguez, Jorge E.
Ramírez, Alfonso E.
Thermal behaviour of romarchite phase SnO in different atmospheres: a hypothesis about the phase transformation
title Thermal behaviour of romarchite phase SnO in different atmospheres: a hypothesis about the phase transformation
title_full Thermal behaviour of romarchite phase SnO in different atmospheres: a hypothesis about the phase transformation
title_fullStr Thermal behaviour of romarchite phase SnO in different atmospheres: a hypothesis about the phase transformation
title_full_unstemmed Thermal behaviour of romarchite phase SnO in different atmospheres: a hypothesis about the phase transformation
title_short Thermal behaviour of romarchite phase SnO in different atmospheres: a hypothesis about the phase transformation
title_sort thermal behaviour of romarchite phase sno in different atmospheres: a hypothesis about the phase transformation
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4946215/
https://www.ncbi.nlm.nih.gov/pubmed/27441283
http://dx.doi.org/10.1016/j.heliyon.2016.e00112
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