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Elemental sulfur coarsening kinetics

BACKGROUND: Elemental sulfur exists is a variety of forms in natural systems, from dissolved forms (noted as S(8(diss)) or in water as S(8(aq))) to bulk elemental sulfur (most stable as α-S(8)). Elemental sulfur can form via several biotic and abiotic processes, many beginning with small sulfur oxid...

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Autores principales: Garcia, Angel A, Druschel, Gregory K
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer International Publishing 2014
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4631715/
https://www.ncbi.nlm.nih.gov/pubmed/26561455
http://dx.doi.org/10.1186/s12932-014-0011-z
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author Garcia, Angel A
Druschel, Gregory K
author_facet Garcia, Angel A
Druschel, Gregory K
author_sort Garcia, Angel A
collection PubMed
description BACKGROUND: Elemental sulfur exists is a variety of forms in natural systems, from dissolved forms (noted as S(8(diss)) or in water as S(8(aq))) to bulk elemental sulfur (most stable as α-S(8)). Elemental sulfur can form via several biotic and abiotic processes, many beginning with small sulfur oxide or polysulfidic sulfur molecules that coarsen into S(8) rings that then coalesce into larger forms: 1. [Formula: see text] Formation of elemental sulfur can be possible via two primary techniques to create an emulsion of liquid sulfur in water called sulfur sols that approximate some mechanisms of possible elemental sulfur formation in natural systems. These techniques produce hydrophobic (S(8(Weimarn))) and hydrophilic (S(8(polysulfide))) sols that exist as nanoparticle and colloidal suspensions. These sols begin as small sulfur oxide or polysulfidic sulfur molecules, or dissolved S(8(aq)) forms, but quickly become nanoparticulate and coarsen into micron sized particles via a combination of classical nucleation, aggregation processes, and/or Ostwald ripening. RESULTS: We conducted a series of experiments to study the rate of elemental sulfur particle coarsening using dynamic light scattering (DLS) analysis under different physical and chemical conditions. Rates of nucleation and initial coarsening occur over seconds to minutes at rates too fast to measure by DLS, with subsequent coarsening of S(8(nano)) and S(8(sol)) being strongly temperature dependent, with rates up to 20 times faster at 75°C compared to 20°C. The addition of surfactants (utilizing ionic and nonionic surfactants as model compounds) results in a significant reduction of coarsening rates, in addition to known effects of these molecules on elemental sulfur solubility. DLS and cryo-SEM results suggest coarsening is largely a product of ripening processes rather than particle aggregation, especially at higher temperatures. Fitting of the coarsening rate data to established models for Ostwald ripening additionally support this as a primary mechanism of coarsening. CONCLUSIONS: Elemental sulfur sols coarsen rapidly at elevated temperatures and experience significant effects on both solubility and particle coarsening kinetics due to interaction with surfactants. Growth of elemental sulfur nanoparticles and sols is largely governed by Ostwald ripening processes. [Image: see text] ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (doi:10.1186/s12932-014-0011-z) contains supplementary material, which is available to authorized users.
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spelling pubmed-46317152015-11-09 Elemental sulfur coarsening kinetics Garcia, Angel A Druschel, Gregory K Geochem Trans Research Article BACKGROUND: Elemental sulfur exists is a variety of forms in natural systems, from dissolved forms (noted as S(8(diss)) or in water as S(8(aq))) to bulk elemental sulfur (most stable as α-S(8)). Elemental sulfur can form via several biotic and abiotic processes, many beginning with small sulfur oxide or polysulfidic sulfur molecules that coarsen into S(8) rings that then coalesce into larger forms: 1. [Formula: see text] Formation of elemental sulfur can be possible via two primary techniques to create an emulsion of liquid sulfur in water called sulfur sols that approximate some mechanisms of possible elemental sulfur formation in natural systems. These techniques produce hydrophobic (S(8(Weimarn))) and hydrophilic (S(8(polysulfide))) sols that exist as nanoparticle and colloidal suspensions. These sols begin as small sulfur oxide or polysulfidic sulfur molecules, or dissolved S(8(aq)) forms, but quickly become nanoparticulate and coarsen into micron sized particles via a combination of classical nucleation, aggregation processes, and/or Ostwald ripening. RESULTS: We conducted a series of experiments to study the rate of elemental sulfur particle coarsening using dynamic light scattering (DLS) analysis under different physical and chemical conditions. Rates of nucleation and initial coarsening occur over seconds to minutes at rates too fast to measure by DLS, with subsequent coarsening of S(8(nano)) and S(8(sol)) being strongly temperature dependent, with rates up to 20 times faster at 75°C compared to 20°C. The addition of surfactants (utilizing ionic and nonionic surfactants as model compounds) results in a significant reduction of coarsening rates, in addition to known effects of these molecules on elemental sulfur solubility. DLS and cryo-SEM results suggest coarsening is largely a product of ripening processes rather than particle aggregation, especially at higher temperatures. Fitting of the coarsening rate data to established models for Ostwald ripening additionally support this as a primary mechanism of coarsening. CONCLUSIONS: Elemental sulfur sols coarsen rapidly at elevated temperatures and experience significant effects on both solubility and particle coarsening kinetics due to interaction with surfactants. Growth of elemental sulfur nanoparticles and sols is largely governed by Ostwald ripening processes. [Image: see text] ELECTRONIC SUPPLEMENTARY MATERIAL: The online version of this article (doi:10.1186/s12932-014-0011-z) contains supplementary material, which is available to authorized users. Springer International Publishing 2014-08-06 /pmc/articles/PMC4631715/ /pubmed/26561455 http://dx.doi.org/10.1186/s12932-014-0011-z Text en © Garcia and Druschel; licensee Chem Central 2014 This article is published under license to BioMed Central Ltd. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited. The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/) applies to the data made available in this article, unless otherwise stated. Open AccessThis article is distributed under the terms of the Creative Commons Attribution 4.0 International License (https://creativecommons.org/licenses/by/4.0), which permits use, duplication, adaptation, distribution, and reproduction in any medium or format, as long as 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 Research Article
Garcia, Angel A
Druschel, Gregory K
Elemental sulfur coarsening kinetics
title Elemental sulfur coarsening kinetics
title_full Elemental sulfur coarsening kinetics
title_fullStr Elemental sulfur coarsening kinetics
title_full_unstemmed Elemental sulfur coarsening kinetics
title_short Elemental sulfur coarsening kinetics
title_sort elemental sulfur coarsening kinetics
topic Research Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4631715/
https://www.ncbi.nlm.nih.gov/pubmed/26561455
http://dx.doi.org/10.1186/s12932-014-0011-z
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