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Characterization of the Vaporization Inlet for Aerosols (VIA) for online measurements of particulate highly oxygenated organic molecules (HOMs)

Particulate matter has major climate and health impacts, and it is therefore of utmost importance to be able to measure the composition of these particles to gain insights into their sources and characteristics. Many methods, both offline and online, have been employed over the years to achieve this...

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Published in:Atmospheric measurement techniques 2024-03, Vol.17 (5), p.1527-1543
Main Authors: Zhao, Jian, Mickwitz, Valter, Luo, Yuanyuan, Häkkinen, Ella, Graeffe, Frans, Zhang, Jiangyi, Timonen, Hilkka, Canagaratna, Manjula, Krechmer, Jordan E., Zhang, Qi, Kulmala, Markku, Kangasluoma, Juha, Worsnop, Douglas, Ehn, Mikael
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container_issue 5
container_start_page 1527
container_title Atmospheric measurement techniques
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creator Zhao, Jian
Mickwitz, Valter
Luo, Yuanyuan
Häkkinen, Ella
Graeffe, Frans
Zhang, Jiangyi
Timonen, Hilkka
Canagaratna, Manjula
Krechmer, Jordan E.
Zhang, Qi
Kulmala, Markku
Kangasluoma, Juha
Worsnop, Douglas
Ehn, Mikael
description Particulate matter has major climate and health impacts, and it is therefore of utmost importance to be able to measure the composition of these particles to gain insights into their sources and characteristics. Many methods, both offline and online, have been employed over the years to achieve this goal. One of the most recent developments is the Vaporization Inlet for Aerosols (VIA) coupled to a nitrate Chemical Ionization Mass Spectrometer (NO3-CIMS), but a thorough understanding of the VIA–NO3-CIMS system remains incomplete. In this work, we ran a series of tests to assess the impacts from different systems and sampling parameters on the detection efficiency of highly oxygenated organic molecules (HOMs) in the VIA–NO3-CIMS system. Firstly, we found that the current VIA system (which includes an activated carbon denuder and a vaporization tube) efficiently transmits particles (> 90 % for particles larger than 50 nm) while also removing gaseous compounds (> 97% for tested volatile organic compounds – VOCs). One of the main differences between the VIA and traditional thermal desorption (TD) techniques is the very short residence time in the heating region, on the order of 0.1 s. We found that this short residence time, and the corresponding short contact with heated surfaces, is likely one of the main reasons why relatively reactive or weakly bound peroxides, for example, were observable using the VIA. However, the VIA also requires much higher temperatures in order to fully evaporate the aerosol components. For example, the evaporation temperature of ammonium sulfate particles using the VIA was found to be about 100–150 °C higher than in typical TD systems. We also observed that the evaporation of particles with larger sizes occurred at slightly higher temperatures compared to smaller particles. Another major aspect that we investigated was the gas-phase wall losses of evaporated molecules. With a more optimized interface between the VIA and the NO3-CIMS, we were able to greatly decrease wall losses and thus improve the sensitivity compared to our earlier VIA work. This interface included a dedicated sheath flow unit to cool the heated sample and provide the NO3-CIMS with the needed high flow (10 L min−1). Our results indicate that most organic molecules observable by the NO3-CIMS can evaporate and be transported efficiently in the VIA system, but upon contact with the hot walls of the VIA, the molecules are instantaneously lost. This loss potentially le
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Many methods, both offline and online, have been employed over the years to achieve this goal. One of the most recent developments is the Vaporization Inlet for Aerosols (VIA) coupled to a nitrate Chemical Ionization Mass Spectrometer (NO3-CIMS), but a thorough understanding of the VIA–NO3-CIMS system remains incomplete. In this work, we ran a series of tests to assess the impacts from different systems and sampling parameters on the detection efficiency of highly oxygenated organic molecules (HOMs) in the VIA–NO3-CIMS system. Firstly, we found that the current VIA system (which includes an activated carbon denuder and a vaporization tube) efficiently transmits particles (&gt; 90 % for particles larger than 50 nm) while also removing gaseous compounds (&gt; 97% for tested volatile organic compounds – VOCs). One of the main differences between the VIA and traditional thermal desorption (TD) techniques is the very short residence time in the heating region, on the order of 0.1 s. We found that this short residence time, and the corresponding short contact with heated surfaces, is likely one of the main reasons why relatively reactive or weakly bound peroxides, for example, were observable using the VIA. However, the VIA also requires much higher temperatures in order to fully evaporate the aerosol components. For example, the evaporation temperature of ammonium sulfate particles using the VIA was found to be about 100–150 °C higher than in typical TD systems. We also observed that the evaporation of particles with larger sizes occurred at slightly higher temperatures compared to smaller particles. Another major aspect that we investigated was the gas-phase wall losses of evaporated molecules. With a more optimized interface between the VIA and the NO3-CIMS, we were able to greatly decrease wall losses and thus improve the sensitivity compared to our earlier VIA work. This interface included a dedicated sheath flow unit to cool the heated sample and provide the NO3-CIMS with the needed high flow (10 L min−1). Our results indicate that most organic molecules observable by the NO3-CIMS can evaporate and be transported efficiently in the VIA system, but upon contact with the hot walls of the VIA, the molecules are instantaneously lost. This loss potentially leads to fragmentation products that are not observable by the NO3-CIMS. Thermograms, obtained by scanning the VIA temperature, were found to be very valuable for both quantification purposes and for estimating the volatility of the evaporating compounds. We developed a simple one-dimensional model to account for the evaporation of particles and the temperature-dependent wall losses of the evaporated molecules, and we thereby estimate the concentration of HOMs in secondary organic aerosol (SOA) particles. Overall, our results provide much-needed insights into the key processes underlying the VIA–NO3-CIMS method. Although there are still some limitations that could be addressed through hardware improvements, the VIA–NO3-CIMS system is a very promising and useful system for fast online measurements of HOMs in the particle phase.</description><identifier>ISSN: 1867-8548</identifier><identifier>ISSN: 1867-1381</identifier><identifier>EISSN: 1867-8548</identifier><identifier>DOI: 10.5194/amt-17-1527-2024</identifier><language>eng</language><publisher>Katlenburg-Lindau: Copernicus GmbH</publisher><subject>Activated carbon ; Aerosols ; Ammonium ; Ammonium compounds ; Ammonium sulfate ; Climate and health ; Decomposition ; Evaporation ; Gases ; High flow ; High temperature ; Inlets ; Investigations ; Ionization ; Mass spectrometry ; One dimensional models ; Organic chemistry ; Organic compounds ; Oxidation ; Oxygenation ; Particulate matter ; Peroxides ; Polyethylene glycol ; Residence time ; Residence time distribution ; Secondary aerosols ; Sheaths ; Sulfate particles ; Sulfates ; Suspended particulate matter ; Temperature dependence ; Vaporization ; VOCs ; Volatile organic compounds</subject><ispartof>Atmospheric measurement techniques, 2024-03, Vol.17 (5), p.1527-1543</ispartof><rights>2024. 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We found that this short residence time, and the corresponding short contact with heated surfaces, is likely one of the main reasons why relatively reactive or weakly bound peroxides, for example, were observable using the VIA. However, the VIA also requires much higher temperatures in order to fully evaporate the aerosol components. For example, the evaporation temperature of ammonium sulfate particles using the VIA was found to be about 100–150 °C higher than in typical TD systems. We also observed that the evaporation of particles with larger sizes occurred at slightly higher temperatures compared to smaller particles. Another major aspect that we investigated was the gas-phase wall losses of evaporated molecules. With a more optimized interface between the VIA and the NO3-CIMS, we were able to greatly decrease wall losses and thus improve the sensitivity compared to our earlier VIA work. This interface included a dedicated sheath flow unit to cool the heated sample and provide the NO3-CIMS with the needed high flow (10 L min−1). Our results indicate that most organic molecules observable by the NO3-CIMS can evaporate and be transported efficiently in the VIA system, but upon contact with the hot walls of the VIA, the molecules are instantaneously lost. This loss potentially leads to fragmentation products that are not observable by the NO3-CIMS. Thermograms, obtained by scanning the VIA temperature, were found to be very valuable for both quantification purposes and for estimating the volatility of the evaporating compounds. We developed a simple one-dimensional model to account for the evaporation of particles and the temperature-dependent wall losses of the evaporated molecules, and we thereby estimate the concentration of HOMs in secondary organic aerosol (SOA) particles. Overall, our results provide much-needed insights into the key processes underlying the VIA–NO3-CIMS method. 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Mickwitz, Valter ; Luo, Yuanyuan ; Häkkinen, Ella ; Graeffe, Frans ; Zhang, Jiangyi ; Timonen, Hilkka ; Canagaratna, Manjula ; Krechmer, Jordan E. ; Zhang, Qi ; Kulmala, Markku ; Kangasluoma, Juha ; Worsnop, Douglas ; Ehn, Mikael</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c332t-e3c2f2cda79a01075763939503f9f8b556aebfdad672e505cd44edecf3ff118d3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2024</creationdate><topic>Activated carbon</topic><topic>Aerosols</topic><topic>Ammonium</topic><topic>Ammonium compounds</topic><topic>Ammonium sulfate</topic><topic>Climate and health</topic><topic>Decomposition</topic><topic>Evaporation</topic><topic>Gases</topic><topic>High flow</topic><topic>High temperature</topic><topic>Inlets</topic><topic>Investigations</topic><topic>Ionization</topic><topic>Mass spectrometry</topic><topic>One dimensional models</topic><topic>Organic chemistry</topic><topic>Organic compounds</topic><topic>Oxidation</topic><topic>Oxygenation</topic><topic>Particulate matter</topic><topic>Peroxides</topic><topic>Polyethylene glycol</topic><topic>Residence time</topic><topic>Residence time distribution</topic><topic>Secondary aerosols</topic><topic>Sheaths</topic><topic>Sulfate particles</topic><topic>Sulfates</topic><topic>Suspended particulate matter</topic><topic>Temperature dependence</topic><topic>Vaporization</topic><topic>VOCs</topic><topic>Volatile organic compounds</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhao, Jian</creatorcontrib><creatorcontrib>Mickwitz, Valter</creatorcontrib><creatorcontrib>Luo, Yuanyuan</creatorcontrib><creatorcontrib>Häkkinen, Ella</creatorcontrib><creatorcontrib>Graeffe, Frans</creatorcontrib><creatorcontrib>Zhang, Jiangyi</creatorcontrib><creatorcontrib>Timonen, Hilkka</creatorcontrib><creatorcontrib>Canagaratna, Manjula</creatorcontrib><creatorcontrib>Krechmer, Jordan E.</creatorcontrib><creatorcontrib>Zhang, Qi</creatorcontrib><creatorcontrib>Kulmala, Markku</creatorcontrib><creatorcontrib>Kangasluoma, Juha</creatorcontrib><creatorcontrib>Worsnop, Douglas</creatorcontrib><creatorcontrib>Ehn, Mikael</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>Meteorological &amp; 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Many methods, both offline and online, have been employed over the years to achieve this goal. One of the most recent developments is the Vaporization Inlet for Aerosols (VIA) coupled to a nitrate Chemical Ionization Mass Spectrometer (NO3-CIMS), but a thorough understanding of the VIA–NO3-CIMS system remains incomplete. In this work, we ran a series of tests to assess the impacts from different systems and sampling parameters on the detection efficiency of highly oxygenated organic molecules (HOMs) in the VIA–NO3-CIMS system. Firstly, we found that the current VIA system (which includes an activated carbon denuder and a vaporization tube) efficiently transmits particles (&gt; 90 % for particles larger than 50 nm) while also removing gaseous compounds (&gt; 97% for tested volatile organic compounds – VOCs). One of the main differences between the VIA and traditional thermal desorption (TD) techniques is the very short residence time in the heating region, on the order of 0.1 s. We found that this short residence time, and the corresponding short contact with heated surfaces, is likely one of the main reasons why relatively reactive or weakly bound peroxides, for example, were observable using the VIA. However, the VIA also requires much higher temperatures in order to fully evaporate the aerosol components. For example, the evaporation temperature of ammonium sulfate particles using the VIA was found to be about 100–150 °C higher than in typical TD systems. We also observed that the evaporation of particles with larger sizes occurred at slightly higher temperatures compared to smaller particles. Another major aspect that we investigated was the gas-phase wall losses of evaporated molecules. With a more optimized interface between the VIA and the NO3-CIMS, we were able to greatly decrease wall losses and thus improve the sensitivity compared to our earlier VIA work. This interface included a dedicated sheath flow unit to cool the heated sample and provide the NO3-CIMS with the needed high flow (10 L min−1). Our results indicate that most organic molecules observable by the NO3-CIMS can evaporate and be transported efficiently in the VIA system, but upon contact with the hot walls of the VIA, the molecules are instantaneously lost. This loss potentially leads to fragmentation products that are not observable by the NO3-CIMS. Thermograms, obtained by scanning the VIA temperature, were found to be very valuable for both quantification purposes and for estimating the volatility of the evaporating compounds. We developed a simple one-dimensional model to account for the evaporation of particles and the temperature-dependent wall losses of the evaporated molecules, and we thereby estimate the concentration of HOMs in secondary organic aerosol (SOA) particles. Overall, our results provide much-needed insights into the key processes underlying the VIA–NO3-CIMS method. Although there are still some limitations that could be addressed through hardware improvements, the VIA–NO3-CIMS system is a very promising and useful system for fast online measurements of HOMs in the particle phase.</abstract><cop>Katlenburg-Lindau</cop><pub>Copernicus GmbH</pub><doi>10.5194/amt-17-1527-2024</doi><tpages>17</tpages><orcidid>https://orcid.org/0000-0001-7304-4651</orcidid><orcidid>https://orcid.org/0000-0003-4253-3596</orcidid><orcidid>https://orcid.org/0000-0002-1639-1187</orcidid><orcidid>https://orcid.org/0000-0003-3642-0659</orcidid><orcidid>https://orcid.org/0000-0003-3464-7825</orcidid><orcidid>https://orcid.org/0009-0007-5244-5334</orcidid><orcidid>https://orcid.org/0000-0002-7987-7985</orcidid><orcidid>https://orcid.org/0000-0002-4894-9587</orcidid><orcidid>https://orcid.org/0000-0002-5203-8778</orcidid><orcidid>https://orcid.org/0000-0002-9571-8925</orcidid><orcidid>https://orcid.org/0000-0002-8803-4007</orcidid><orcidid>https://orcid.org/0000-0002-0215-4893</orcidid><oa>free_for_read</oa></addata></record>
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identifier ISSN: 1867-8548
ispartof Atmospheric measurement techniques, 2024-03, Vol.17 (5), p.1527-1543
issn 1867-8548
1867-1381
1867-8548
language eng
recordid cdi_doaj_primary_oai_doaj_org_article_a9106fc953854777af6bd9743e20ddff
source Publicly Available Content Database; DOAJ Directory of Open Access Journals
subjects Activated carbon
Aerosols
Ammonium
Ammonium compounds
Ammonium sulfate
Climate and health
Decomposition
Evaporation
Gases
High flow
High temperature
Inlets
Investigations
Ionization
Mass spectrometry
One dimensional models
Organic chemistry
Organic compounds
Oxidation
Oxygenation
Particulate matter
Peroxides
Polyethylene glycol
Residence time
Residence time distribution
Secondary aerosols
Sheaths
Sulfate particles
Sulfates
Suspended particulate matter
Temperature dependence
Vaporization
VOCs
Volatile organic compounds
title Characterization of the Vaporization Inlet for Aerosols (VIA) for online measurements of particulate highly oxygenated organic molecules (HOMs)
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