Thermal–optical analysis of quartz fiber filters loaded with snow samples – determination of iron based on interferences caused by mineral dust

<p>The determination of mineral dust and elemental carbon in snow samples is of great interest, since both compounds are known to be light-absorbing snow impurities. Different analytical methods have to be used to quantify both compounds. The occurrence of mineral dust, which contains hematite...

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Main Authors: D. Kau, M. Greilinger, B. Kirchsteiger, A. Göndör, C. Herzig, A. Limbeck, E. Eitenberger, A. Kasper-Giebl
Format: Article
Language:English
Published: Copernicus Publications 2022-09-01
Series:Atmospheric Measurement Techniques
Online Access:https://amt.copernicus.org/articles/15/5207/2022/amt-15-5207-2022.pdf
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author D. Kau
M. Greilinger
B. Kirchsteiger
A. Göndör
C. Herzig
A. Limbeck
E. Eitenberger
A. Kasper-Giebl
author_facet D. Kau
M. Greilinger
B. Kirchsteiger
A. Göndör
C. Herzig
A. Limbeck
E. Eitenberger
A. Kasper-Giebl
author_sort D. Kau
collection DOAJ
description <p>The determination of mineral dust and elemental carbon in snow samples is of great interest, since both compounds are known to be light-absorbing snow impurities. Different analytical methods have to be used to quantify both compounds. The occurrence of mineral dust, which contains hematite, leads to a bias in the quantification of elemental carbon and organic carbon via thermal–optical analysis. Here we present an approach which utilizes this interference to determine the concentration of iron via thermal–optical analysis using a Lab OC <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="1b4178c77ca0d4bfee6c9ddd864f3a43"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-15-5207-2022-ie00001.svg" width="8pt" height="14pt" src="amt-15-5207-2022-ie00001.png"/></svg:svg></span></span> EC Aerosol Analyzer (Sunset Laboratory Inc.) and the EUSAAR2 protocol. For this, the temperature dependency of the transmittance signal determined during the calibration phase, i.e., when all carbonaceous compounds are already removed, is evaluated. Converting the transmittance signal into an attenuation, a linear relationship between this attenuation and the iron loading is obtained for loadings ranging from 10 to 100 <span class="inline-formula">µ</span>g Fe cm<span class="inline-formula"><sup>−2</sup></span>. Furthermore, evaluation of the transmittance signal during the calibration phase allows to identify samples which need to be re-evaluated, since the analysis of elemental carbon and organic carbon is biased by constituents of mineral dust. The method, which was initially designed for snow samples, can also be used to evaluate particulate matter samples collected within the same high alpine environment. When applying the method to a new set of samples it is crucial to check whether the composition of iron compounds and the sample matrix remain comparable. If other sources than mineral dust determine the iron concentration in particulate matter, these samples cannot be evaluated with thermal–optical analysis. This is shown exemplarily with data from particulate matter samples collected in a railway tunnel.</p>
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spelling doaj.art-f47f8d0b18b34050947d62f703029d662022-12-22T04:04:46ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482022-09-01155207521710.5194/amt-15-5207-2022Thermal–optical analysis of quartz fiber filters loaded with snow samples – determination of iron based on interferences caused by mineral dustD. Kau0M. Greilinger1B. Kirchsteiger2A. Göndör3C. Herzig4A. Limbeck5E. Eitenberger6A. Kasper-Giebl7Institute of Technologies and Analytics, TU Wien, Vienna, 1060, AustriaSection Climate Monitoring and Cryosphere, Zentralanstalt für Meteorologie und Geodynamik (ZAMG), Vienna, 1190, Austria​​​​​​​Institute of Technologies and Analytics, TU Wien, Vienna, 1060, AustriaInstitute of Technologies and Analytics, TU Wien, Vienna, 1060, AustriaInstitute of Technologies and Analytics, TU Wien, Vienna, 1060, AustriaInstitute of Technologies and Analytics, TU Wien, Vienna, 1060, AustriaInstitute of Technologies and Analytics, TU Wien, Vienna, 1060, AustriaInstitute of Technologies and Analytics, TU Wien, Vienna, 1060, Austria<p>The determination of mineral dust and elemental carbon in snow samples is of great interest, since both compounds are known to be light-absorbing snow impurities. Different analytical methods have to be used to quantify both compounds. The occurrence of mineral dust, which contains hematite, leads to a bias in the quantification of elemental carbon and organic carbon via thermal–optical analysis. Here we present an approach which utilizes this interference to determine the concentration of iron via thermal–optical analysis using a Lab OC <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="1b4178c77ca0d4bfee6c9ddd864f3a43"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="amt-15-5207-2022-ie00001.svg" width="8pt" height="14pt" src="amt-15-5207-2022-ie00001.png"/></svg:svg></span></span> EC Aerosol Analyzer (Sunset Laboratory Inc.) and the EUSAAR2 protocol. For this, the temperature dependency of the transmittance signal determined during the calibration phase, i.e., when all carbonaceous compounds are already removed, is evaluated. Converting the transmittance signal into an attenuation, a linear relationship between this attenuation and the iron loading is obtained for loadings ranging from 10 to 100 <span class="inline-formula">µ</span>g Fe cm<span class="inline-formula"><sup>−2</sup></span>. Furthermore, evaluation of the transmittance signal during the calibration phase allows to identify samples which need to be re-evaluated, since the analysis of elemental carbon and organic carbon is biased by constituents of mineral dust. The method, which was initially designed for snow samples, can also be used to evaluate particulate matter samples collected within the same high alpine environment. When applying the method to a new set of samples it is crucial to check whether the composition of iron compounds and the sample matrix remain comparable. If other sources than mineral dust determine the iron concentration in particulate matter, these samples cannot be evaluated with thermal–optical analysis. This is shown exemplarily with data from particulate matter samples collected in a railway tunnel.</p>https://amt.copernicus.org/articles/15/5207/2022/amt-15-5207-2022.pdf
spellingShingle D. Kau
M. Greilinger
B. Kirchsteiger
A. Göndör
C. Herzig
A. Limbeck
E. Eitenberger
A. Kasper-Giebl
Thermal–optical analysis of quartz fiber filters loaded with snow samples – determination of iron based on interferences caused by mineral dust
Atmospheric Measurement Techniques
title Thermal–optical analysis of quartz fiber filters loaded with snow samples – determination of iron based on interferences caused by mineral dust
title_full Thermal–optical analysis of quartz fiber filters loaded with snow samples – determination of iron based on interferences caused by mineral dust
title_fullStr Thermal–optical analysis of quartz fiber filters loaded with snow samples – determination of iron based on interferences caused by mineral dust
title_full_unstemmed Thermal–optical analysis of quartz fiber filters loaded with snow samples – determination of iron based on interferences caused by mineral dust
title_short Thermal–optical analysis of quartz fiber filters loaded with snow samples – determination of iron based on interferences caused by mineral dust
title_sort thermal optical analysis of quartz fiber filters loaded with snow samples determination of iron based on interferences caused by mineral dust
url https://amt.copernicus.org/articles/15/5207/2022/amt-15-5207-2022.pdf
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