TY - JOUR
T1 - Evaluation and Inter-Comparison of Oxygen-Based OC-EC Separation Methods for Radiocarbon Analysis of Ambient Aerosol Particle Samples
AU - Zenker, Katrin
AU - Vonwiller, Matthias
AU - Szidat, Sonke
AU - Calzolai, Giulia
AU - Giannoni, Martina
AU - Bernardoni, Vera
AU - Jedynska, Aleksandra D.
AU - Henzing, Bas
AU - Meijer, Harro A. J.
AU - Dusek, Ulrike
PY - 2017/11/21
Y1 - 2017/11/21
N2 - Radiocarbon analysis is a widely-used tool for source apportionment of aerosol particles. One of the big challenges of this method, addressed in this work, is to isolate elemental carbon (EC) for C-14 analysis. In the first part of the study, we validate a two-step method (2stepCIO) to separate total carbon (TC) into organic carbon (OC) and EC against the EUSAAR_2 thermal-optical method regarding the recovered carbon concentrations. The 2stepCIO method is based on the combustion of OC in pure oxygen at two different temperature steps to isolate EC. It is normally used with a custom-built aerosol combustion system (ACS), but in this project, it was also implemented as a thermal protocol on a Sunset OC-EC analyzer. Results for the recovered EC mass concentration showed poor agreement between the 2stepCIO method on the ACS system and on the Sunset analyzer. This indicates that the EC recovery is sensitive not only to the temperature steps, but also to instrument-specific parameters, such as heating rates. We also found that the EUSAAR_2 protocol itself can underestimate the EC concentration on untreated samples compared to water-extracted samples. This is especially so for highly loaded filters, which are typical for C-14 analysis. For untreated samples, the EC concentration on long-term filter samples (two to five days sampling time) was 20-45% lower than the sum of EC found on the corresponding 24-h filter samples. For water-extracted filter samples, there was no significant difference between long-term and the sum of daily filter samples. In the second part of this study, the C-14 was measured on EC isolated by the 2stepCIO method and compared to methods from two other laboratories. The different methods agree well within their uncertainty estimates.
AB - Radiocarbon analysis is a widely-used tool for source apportionment of aerosol particles. One of the big challenges of this method, addressed in this work, is to isolate elemental carbon (EC) for C-14 analysis. In the first part of the study, we validate a two-step method (2stepCIO) to separate total carbon (TC) into organic carbon (OC) and EC against the EUSAAR_2 thermal-optical method regarding the recovered carbon concentrations. The 2stepCIO method is based on the combustion of OC in pure oxygen at two different temperature steps to isolate EC. It is normally used with a custom-built aerosol combustion system (ACS), but in this project, it was also implemented as a thermal protocol on a Sunset OC-EC analyzer. Results for the recovered EC mass concentration showed poor agreement between the 2stepCIO method on the ACS system and on the Sunset analyzer. This indicates that the EC recovery is sensitive not only to the temperature steps, but also to instrument-specific parameters, such as heating rates. We also found that the EUSAAR_2 protocol itself can underestimate the EC concentration on untreated samples compared to water-extracted samples. This is especially so for highly loaded filters, which are typical for C-14 analysis. For untreated samples, the EC concentration on long-term filter samples (two to five days sampling time) was 20-45% lower than the sum of EC found on the corresponding 24-h filter samples. For water-extracted filter samples, there was no significant difference between long-term and the sum of daily filter samples. In the second part of this study, the C-14 was measured on EC isolated by the 2stepCIO method and compared to methods from two other laboratories. The different methods agree well within their uncertainty estimates.
KW - radiocarbon
KW - organic carbon
KW - elemental carbon
KW - carbonaceous aerosol particles
KW - thermal separation
KW - C-14-BASED SOURCE ASSESSMENT
KW - THERMAL-OPTICAL PROTOCOL
KW - REGIONAL BACKGROUND SITE
KW - ELEMENTAL CARBON
KW - BLACK CARBON
KW - SOURCE APPORTIONMENT
KW - PARTICULATE MATTER
KW - ORGANIC-CARBON
KW - ATMOSPHERIC AEROSOLS
KW - DIURNAL-VARIATIONS
U2 - 10.3390/atmos8110226
DO - 10.3390/atmos8110226
M3 - Article
SN - 2073-4433
VL - 8
JO - Atmosphere
JF - Atmosphere
IS - 11
M1 - 226
ER -