Preprints
https://doi.org/10.5194/egusphere-2023-2216
https://doi.org/10.5194/egusphere-2023-2216
06 Oct 2023
 | 06 Oct 2023

Comparison of the LEO and CPMA-SP2 techniques for black-carbon mixing-state measurements

Arash Naseri, Joel Corbin, and Jason Olfert

Abstract. It is necessary to measure the mixing states of light-absorbing carbon (LAC) particles to reduce uncertainties in climate forcing due to particulate from wildfires and biomass combustion. For refractory LAC (normally called refractory black carbon; rBC), such measurements can be made using the single particle soot photometer (SP2). The SP2 measures the incandescent mass of individual particles due to heating by a 1064 nm laser. The SP2 also monitors single-particle light scattering from rBC plus internally mixed material (e.g., coatings of volatile particulate matter). rBC mixing states can be estimated from SP2 measurements by combining the scattering and incandescence signals. This is the basis of the published methods known as the (i ) scattering–incandescence lag-time, (ii ) leading-edge only (LEO), and (iii ) normalized derivative methods. More recently, the tandem centrifugal particle mass analyzer (CPMA)–SP2 method has been developed. The CPMA–SP2 method does not rely on the SP2 scattering signals and, therefore truly measures the rBC mass fraction, with no assumptions regarding particle composition or morphology. In this study, we provide the first quantitative comparison of the light-scattering and CPMA–SP2 methods for measuring mixing state. We discuss the upper and lower limits of detection (in terms of both rBC and coatings), temporal resolution, role of counting statistics, and errors associated with the measurements. We use a data set of atmospheric particles sampled at a regional background site (Kamloops, Canada; about 350 km northeast of Vancouver, British Columbia, Canada), where the majority of rBC was emitted by seasonal wildfires. In the overall comparison among measurement methods, the CPMA–SP2 method is found to have significantly better systematic uncertainties than the light-scattering methods for wildfire smoke. For example, the light-scattering methods could not quantify coatings on half of the rBC particles, because their light-scattering signals were below the SP2 detection limit. Consequently, the bias in SP2-only estimates of rBC mixing states depends on the size distribution of the rBC particles. Although more accurate, CPMA–SP2 measurements require significantly more time to acquire, whereas SP2-only light-scattering analyses (both LEO and lag-time) can provide near real-time qualitative information representing large rBC particles.

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Arash Naseri, Joel Corbin, and Jason Olfert

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-2216', Anonymous Referee #1, 16 Nov 2023
    • AC1: 'Reply on RC1', Arash Naseri, 21 Dec 2023
  • RC2: 'Comment on egusphere-2023-2216', Anonymous Referee #2, 26 Nov 2023
    • AC2: 'Reply on RC2', Arash Naseri, 21 Dec 2023

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-2216', Anonymous Referee #1, 16 Nov 2023
    • AC1: 'Reply on RC1', Arash Naseri, 21 Dec 2023
  • RC2: 'Comment on egusphere-2023-2216', Anonymous Referee #2, 26 Nov 2023
    • AC2: 'Reply on RC2', Arash Naseri, 21 Dec 2023
Arash Naseri, Joel Corbin, and Jason Olfert
Arash Naseri, Joel Corbin, and Jason Olfert

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Latest update: 19 Jun 2024
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Short summary
It is necessary to measure the mixing states of light-absorbing carbon particles to reduce uncertainties in climate forcing caused by particulate matter from wildfires and biomass combustion. This study compares methods for measuring light-absorbing carbon in the atmosphere. The CPMA-SP2 method offers more accurate results than traditional light-scattering methods, such as the leading-edge only (LEO) method, thereby enhancing the accuracy of measuring the mixing states of light-absorbing carbon.