Characterization of the Sunset Semi-Continuous Carbon Aerosol Analyzer

The field-deployable Sunset Semi-Continuous Organic Carbon/Elemental Carbon (Sunset OCEC) aerosol analyzer utilizes the modified National Institute for Occupational Safety and Health thermal-optical method to determine total carbon (TC), organic carbon (OC), and elemental carbon (EC) at near real-ti...

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Published inJournal of the Air & Waste Management Association Vol. 59; no. 7; pp. 826 - 833
Main Authors Bauer, Jace J., Yu, Xiao-Ying, Cary, Robert, Laulainen, Nels, Berkowitz, Carl
Format Journal Article
LanguageEnglish
Published United States Taylor & Francis Group 01.07.2009
Air and Waste Management Association
Taylor & Francis Ltd
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Abstract The field-deployable Sunset Semi-Continuous Organic Carbon/Elemental Carbon (Sunset OCEC) aerosol analyzer utilizes the modified National Institute for Occupational Safety and Health thermal-optical method to determine total carbon (TC), organic carbon (OC), and elemental carbon (EC) at near real-time. Two sets of OC and EC are available: thermal OC and EC, and optical OC and EC. The former is obtained by the thermal-optical approach, and the latter is obtained by directly determining EC optically and deriving optical OC from TC. However, the performance of the Sunset OCEC is not yet fully characterized. Two collocated Sunset OCEC analyzers, Unit A and Unit B, were used to determine the pooled relative standard deviation (RSD) and limit of detection (LOD) between September 18 and November 6, 2007 in Richland, WA. The LOD of Unit A was approximately 0.2 μgC/m 3 (0.1 μgC/cm 2 ) for TC, optical OC, and thermal OC, and 0.01 μgC/m 3 (0.01 μgC/cm 2 ) for optical EC. Similarly, Unit B had an LOD of approximately 0.3 μgC/m 3 (0.2 μgC/cm 2 ) for TC, optical OC, and thermal OC, and 0.02 μgC/m 3 (0.01 μgC/cm 2 ) for optical EC. The LOD for thermal EC is estimated to be 0.2 μgC/m 3 (0.1 μgC/cm 2 ) for both units. The pooled RSDs were 4.9% for TC (carbon mass loadings 0.6-6.0 μgC/cm 2 ), 5.6% for optical OC (carbon mass loadings 0.6-5.4 μgC/cm 2 ), 5.3% for thermal OC (carbon mass loadings 0.6-5.3 μgC/cm 2 ), and 9.6% for optical EC (carbon mass loadings 0-1.4 μgC/cm 2 ), which indicates good precision between the instruments. The RSD for thermal EC is higher at 24.3% (carbon mass loadings 0-1.2 μgC/cm 2 ). Low EC mass loadings in Richland contributed to the poor RSD of EC. The authors found that excessive noise from the nondispersive infrared (NDIR) laser in the Sunset OCEC analyzer could result in a worsened determination of OC and EC. It is recommended that a "quieter" NDIR laser and detector be used in the Sunset OCEC analyzer to improve quantification. Future work should re-evaluate the precision of the EC parameters in an environment favorable for EC collection. Investigation among quantification differences using various thermal-optical protocols to determine OC and EC is also in need.
AbstractList The field-deployable Sunset Semi-Continuous Organic Carbon/Elemental Carbon (Sunset OCEC) aerosol analyzer utilizes the modified National Institute for Occupational Safety and Health thermal-optical method to determine total carbon (TC), organic carbon (OC), and elemental carbon (EC) at near real-time. Two sets of OC and EC are available: thermal OC and EC, and optical OC and EC. The former is obtained by the thermal-optical approach, and the latter is obtained by directly determining EC optically and deriving optical OC from TC. However, the performance of the Sunset OCEC is not yet fully characterized. Two collocated Sunset OCEC analyzers, Unit A and Unit B, were used to determine the pooled relative standard deviation (RSD) and limit of detection (LOD) between September 18 and November 6, 2007 in Richland, WA. The LOD of Unit A was approximately 0.2 µgC/m^sup 3^ (0.1 µgC/cm^sup 2^) for TC, optical OC, and thermal OC, and 0.01 µgC/m^sup 3^ (0.01 µgC/cm^sup 2^) for optical EC. Similarly, Unit B had an LOD of approximately 0.3 µgC/m^sup 3^ (0.2 µgC/cm^sup 2^) for TC, optical OC, and thermal OC, and 0.02 µgC/m^sup 3^ (0.01 µgC/cm^sup 2^) for optical EC. The LOD for thermal EC is estimated to be 0.2 µgC/m^sup 3^ (0.1 µgC/cm^sup 2^) for both units. The pooled RSDs were 4.9% for TC (carbon mass loadings 0.6-6.0 µgC/cm^sup 2^), 5.6% for optical OC (carbon mass loadings 0.6-5.4 µgC/cm^sup 2^), 5.3% for thermal OC (carbon mass loadings 0.6-5.3 µgC/cm^sup 2^), and 9.6% for optical EC (carbon mass loadings 0-1.4 µgC/cm^sup 2^), which indicates good precision between the instruments. The RSD for thermal EC is higher at 24.3% (carbon mass loadings 0-1.2 µgC/cm^sup 2^). Low EC mass loadings in Richland contributed to the poor RSD of EC. The authors found that excessive noise from the nondispersive infrared (NDIR) laser in the Sunset OCEC analyzer could result in a worsened determination of OC and EC. It is recommended that a "quieter" NDIR laser and detector be used in the Sunset OCEC analyzer to improve quantification. Future work should re-evaluate the precision of the EC parameters in an environment favorable for EC collection. Investigation among quantification differences using various thermal-optical protocols to determine OC and EC is also in need. [PUBLICATION ABSTRACT]
The field-deployable Sunset Semi-Continuous Organic Carbon/Elemental Carbon (Sunset OCEC) aerosol analyzer utilizes the modified National Institute for Occupational Safety and Health thermal-optical method to determine total carbon (TC), organic carbon (OC), and elemental carbon (EC) at near real-time. Two sets of OC and EC are available: thermal OC and EC, and optical OC and EC. The former is obtained by the thermal-optical approach, and the latter is obtained by directly determining EC optically and deriving optical OC from TC. However, the performance of the Sunset OCEC is not yet fully characterized. Two collocated Sunset OCEC analyzers, Unit A and Unit B, were used to determine the pooled relative standard deviation (RSD) and limit of detection (LOD) between September 18 and November 6, 2007 in Richland, WA. The LOD of Unit A was approximately 0.2 μgC/m 3 (0.1 μgC/cm 2 ) for TC, optical OC, and thermal OC, and 0.01 μgC/m 3 (0.01 μgC/cm 2 ) for optical EC. Similarly, Unit B had an LOD of approximately 0.3 μgC/m 3 (0.2 μgC/cm 2 ) for TC, optical OC, and thermal OC, and 0.02 μgC/m 3 (0.01 μgC/cm 2 ) for optical EC. The LOD for thermal EC is estimated to be 0.2 μgC/m 3 (0.1 μgC/cm 2 ) for both units. The pooled RSDs were 4.9% for TC (carbon mass loadings 0.6-6.0 μgC/cm 2 ), 5.6% for optical OC (carbon mass loadings 0.6-5.4 μgC/cm 2 ), 5.3% for thermal OC (carbon mass loadings 0.6-5.3 μgC/cm 2 ), and 9.6% for optical EC (carbon mass loadings 0-1.4 μgC/cm 2 ), which indicates good precision between the instruments. The RSD for thermal EC is higher at 24.3% (carbon mass loadings 0-1.2 μgC/cm 2 ). Low EC mass loadings in Richland contributed to the poor RSD of EC. The authors found that excessive noise from the nondispersive infrared (NDIR) laser in the Sunset OCEC analyzer could result in a worsened determination of OC and EC. It is recommended that a "quieter" NDIR laser and detector be used in the Sunset OCEC analyzer to improve quantification. Future work should re-evaluate the precision of the EC parameters in an environment favorable for EC collection. Investigation among quantification differences using various thermal-optical protocols to determine OC and EC is also in need.
The field-deployable Sunset Semi-Continuous Organic Carbon/Elemental Carbon (Sunset OCEC) aerosol analyzer utilizes the modified National Institute for Occupational Safety and Health thermal-optical method to determine total carbon (TC), organic carbon (OC), and elemental carbon (EC) at near real-time. Two sets of OC and EC are available: thermal OC and EC, and optical OC and EC. The former is obtained by the thermal-optical approach, and the latter is obtained by directly determining EC optically and deriving optical OC from TC. However, the performance of the Sunset OCEC is not yet fully characterized. Two collocated Sunset OCEC analyzers, Unit A and Unit B, were used to determine the pooled relative standard deviation (RSD) and limit of detection (LOD) between September 18 and November 6, 2007 in Richland, WA. The LOD of Unit A was approximately 0.2 microgC/m3 (0.1 microgC/cm2) for TC, optical OC, and thermal OC, and 0.01 microgC/m3 (0.01 microgC/cm2) for optical EC. Similarly, Unit B had an LOD of approximately 0.3 microgC/m3 (0.2 microgC/cm2) for TC, optical OC, and thermal OC, and 0.02 microgC/m3 (0.01 microgC/cm2) for optical EC. The LOD for thermal EC is estimated to be 0.2 microgC/m3 (0.1 microgC/cm2) for both units. The pooled RSDs were 4.9% for TC (carbon mass loadings 0.6-6.0 microgC/cm2), 5.6% for optical OC (carbon mass loadings 0.6-5.4 microgC/cm2), 5.3% for thermal OC (carbon mass loadings 0.6-5.3 microgC/ cm2), and 9.6% for optical EC (carbon mass loadings 0-1.4 microgC/cm2), which indicates good precision between the instruments. The RSD for thermal EC is higher at 24.3% (carbon mass loadings 0-1.2 microgC/cm2). Low EC mass loadings in Richland contributed to the poor RSD of EC. The authors found that excessive noise from the nondispersive infrared (NDIR) laser in the Sunset OCEC analyzer could result in a worsened determination of OC and EC. It is recommended that a "quieter" NDIR laser and detector be used in the Sunset OCEC analyzer to improve quantification. Future work should re-evaluate the precision of the EC parameters in an environment favorable for EC collection. Investigation among quantification differences using various thermal-optical protocols to determine OC and EC is also in need.
The field-deployable Sunset Semi-Continuous Organic Carbon/Elemental Carbon (Sunset OCEC) aerosol analyzer utilizes the modified National Institute for Occupational Safety and Health thermal-optical method to determine total carbon (TC), organic carbon (OC), and elemental carbon (EC) at near real-time. Two sets of OC and EC are available: thermal OC and EC, and optical OC and EC. The former is obtained by the thermal-optical approach, and the latter is obtained by directly determining EC optically and deriving optical OC from TC. However, the performance of the Sunset OCEC is not yet fully characterized. Two collocated Sunset OCEC analyzers, Unit A and Unit B, were used to determine the pooled relative standard deviation (RSD) and limit of detection (LOD) between September 18 and November 6,2007 in Richland, WA. The LOD of Unit A was approximately 0.2 ugC/m3 (0.1 ugC/cm2) for TC, optical OC, and thermal OC, and 0.01 ugC/m3 (0.01 ugC/cm2) for optical EC. Similarly, Unit B had an LOD of approximately 0.3 ugC/m3 (0.2 ugC/cm2) for TC, optical OC, and thermal OC, and 0.02 ugC/m3 (0.01 ugC/cm2) for optical EC. The LOD for thermal EC is estimated to be 0.2 ugC/m3 (0.1 ugC/cm2) for both units. The pooled RSDs were 4.9% for TC (carbon mass loadings 0.6-6.0 ugC/cm2), 5.6% for optical OC (carbon mass loadings 0.6-5.4 ugC/cm2), 5.3% for thermal OC (carbon mass loadings 0.6-5.3 ugC/ cm2), and 9.6% for optical EC (carbon mass loadings 0-1.4 ugC/cm2), which indicates good precision between the instruments. The RSD for thermal EC is higher at 24.3% (carbon mass loadings 0-1.2 ugC/cm2). Low EC mass loadings in Richland contributed to the poor RSD of EC. The authors found that excessive noise from the nondispersive infrared (NDIR) laser in the Sunset OCEC analyzer could result in a worsened determination of OC and EC. It is recommended that a 'quieter' NDIR laser and detector be used in the Sunset OCEC analyzer to improve quantification. Future work should re-evaluate the precision of the EC parameters in an environment favorable for EC collection. Investigation among quantification differences using various thermal-optical protocols to determine OC and EC is also in need.
Audience Academic
Author Yu, Xiao-Ying
Bauer, Jace J.
Laulainen, Nels
Berkowitz, Carl
Cary, Robert
Author_xml – sequence: 1
  givenname: Jace J.
  surname: Bauer
  fullname: Bauer, Jace J.
  organization: Department of Earth and Atmospheric Sciences , Purdue University
– sequence: 2
  givenname: Xiao-Ying
  surname: Yu
  fullname: Yu, Xiao-Ying
  email: xiaoying.yu@pnl.gov.
  organization: Atmospheric Science and Global Change Division , Pacific Northwest National Laboratory
– sequence: 3
  givenname: Robert
  surname: Cary
  fullname: Cary, Robert
  organization: Sunset Laboratory, Inc
– sequence: 4
  givenname: Nels
  surname: Laulainen
  fullname: Laulainen, Nels
  organization: Atmospheric Science and Global Change Division , Pacific Northwest National Laboratory
– sequence: 5
  givenname: Carl
  surname: Berkowitz
  fullname: Berkowitz, Carl
  organization: Atmospheric Science and Global Change Division , Pacific Northwest National Laboratory
BackLink https://www.ncbi.nlm.nih.gov/pubmed/19645267$$D View this record in MEDLINE/PubMed
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Cites_doi 10.1002/9780470773666
10.1017/CBO9780511546013
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PublicationTitle Journal of the Air & Waste Management Association
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Snippet The field-deployable Sunset Semi-Continuous Organic Carbon/Elemental Carbon (Sunset OCEC) aerosol analyzer utilizes the modified National Institute for...
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SubjectTerms Aerosols
Aerosols - analysis
Air Pollutants - analysis
Air Pollutants - chemistry
Analytical instruments
Carbon
Carbon - analysis
Carbon compounds
Carbon dioxide
Climate change
Collection
Data collection
Detectors
Environmental monitoring
Environmental Monitoring - instrumentation
Gases
Health
Infrared
Lasers
Measurement
Methods
Noise
Occupational safety
Particulate Matter - analysis
Particulate Matter - chemistry
Protocol
Real time
Reproducibility of Results
Standard deviation
Sunset
Title Characterization of the Sunset Semi-Continuous Carbon Aerosol Analyzer
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