Structural changes of CAST soot during a thermal–optical measurement protocol

<p>Thermal–optical measurement techniques are widely used to classify carbonaceous material. The results of different methods for total carbon are comparable but can vary by <span class="inline-formula">&gt;44</span>&thinsp;% for elemental carbon. One major cause...

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Main Authors: T. Haller, C. Rentenberger, J. C. Meyer, L. Felgitsch, H. Grothe, R. Hitzenberger
Format: Article
Language:English
Published: Copernicus Publications 2019-07-01
Series:Atmospheric Measurement Techniques
Online Access:https://www.atmos-meas-tech.net/12/3503/2019/amt-12-3503-2019.pdf
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author T. Haller
C. Rentenberger
J. C. Meyer
L. Felgitsch
H. Grothe
R. Hitzenberger
author_facet T. Haller
C. Rentenberger
J. C. Meyer
L. Felgitsch
H. Grothe
R. Hitzenberger
author_sort T. Haller
collection DOAJ
description <p>Thermal–optical measurement techniques are widely used to classify carbonaceous material. The results of different methods for total carbon are comparable but can vary by <span class="inline-formula">&gt;44</span>&thinsp;% for elemental carbon. One major cause of variation is the formation of pyrolyzed carbon during the heating process which occurs mainly in samples with a high amount of brown carbon (BrC). In this study the structural changes of two different CAST (combustion aerosol standard) aerosol samples caused by the heating procedure in a thermal–optical instrument were investigated with UV–VIS and Raman spectroscopy, the integrating-sphere technique (IS) and transmission electron microscopy. All analysis techniques showed significant structural changes for BrC-rich samples at the highest temperature level (870&thinsp;<span class="inline-formula"><sup>∘</sup>C</span>) in helium. The structure of the heated BrC-rich sample resembles the structure of an unheated BrC-poor sample. Heating the BrC-rich sample to 870&thinsp;<span class="inline-formula"><sup>∘</sup>C</span> increases the graphitic domain size within the material from 1.6 to 2&thinsp;<span class="inline-formula">nm</span>. Although the Raman spectra unambiguously show this increase in ordering only at the highest temperature step, UV–VIS and IS analyses show a continuous change in the optical properties also at lower temperatures. The sample with a negligible amount of BrC, however, did not show any significant structural changes during the whole heating procedure.</p>
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spelling doaj.art-72ffac5f85cb46ccad909edce92042032022-12-22T00:31:53ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482019-07-01123503351910.5194/amt-12-3503-2019Structural changes of CAST soot during a thermal–optical measurement protocolT. Haller0C. Rentenberger1J. C. Meyer2L. Felgitsch3H. Grothe4R. Hitzenberger5Faculty of Physics, University of Vienna, Vienna, 1090, AustriaFaculty of Physics, University of Vienna, Vienna, 1090, AustriaFaculty of Physics, University of Vienna, Vienna, 1090, AustriaInstitute of Materials Chemistry, TU Wien, Vienna, 1060, AustriaInstitute of Materials Chemistry, TU Wien, Vienna, 1060, AustriaFaculty of Physics, University of Vienna, Vienna, 1090, Austria<p>Thermal–optical measurement techniques are widely used to classify carbonaceous material. The results of different methods for total carbon are comparable but can vary by <span class="inline-formula">&gt;44</span>&thinsp;% for elemental carbon. One major cause of variation is the formation of pyrolyzed carbon during the heating process which occurs mainly in samples with a high amount of brown carbon (BrC). In this study the structural changes of two different CAST (combustion aerosol standard) aerosol samples caused by the heating procedure in a thermal–optical instrument were investigated with UV–VIS and Raman spectroscopy, the integrating-sphere technique (IS) and transmission electron microscopy. All analysis techniques showed significant structural changes for BrC-rich samples at the highest temperature level (870&thinsp;<span class="inline-formula"><sup>∘</sup>C</span>) in helium. The structure of the heated BrC-rich sample resembles the structure of an unheated BrC-poor sample. Heating the BrC-rich sample to 870&thinsp;<span class="inline-formula"><sup>∘</sup>C</span> increases the graphitic domain size within the material from 1.6 to 2&thinsp;<span class="inline-formula">nm</span>. Although the Raman spectra unambiguously show this increase in ordering only at the highest temperature step, UV–VIS and IS analyses show a continuous change in the optical properties also at lower temperatures. The sample with a negligible amount of BrC, however, did not show any significant structural changes during the whole heating procedure.</p>https://www.atmos-meas-tech.net/12/3503/2019/amt-12-3503-2019.pdf
spellingShingle T. Haller
C. Rentenberger
J. C. Meyer
L. Felgitsch
H. Grothe
R. Hitzenberger
Structural changes of CAST soot during a thermal–optical measurement protocol
Atmospheric Measurement Techniques
title Structural changes of CAST soot during a thermal–optical measurement protocol
title_full Structural changes of CAST soot during a thermal–optical measurement protocol
title_fullStr Structural changes of CAST soot during a thermal–optical measurement protocol
title_full_unstemmed Structural changes of CAST soot during a thermal–optical measurement protocol
title_short Structural changes of CAST soot during a thermal–optical measurement protocol
title_sort structural changes of cast soot during a thermal optical measurement protocol
url https://www.atmos-meas-tech.net/12/3503/2019/amt-12-3503-2019.pdf
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