The DOI matches its Crossref record; 31 of the 31 references it cites were found in a registry or an index.
Effects of Mixing State on Black Carbon Measurements by Laser-Induced Incandescence
Open accessAbstract
Laboratory experiments and theoretical calculations were made to characterize the performance of a Single Particle Soot Photometer (SP2) manufactured by Droplet Measurement Technologies (DMT), which was designed to measure the mass and the mixing state of individual black carbon (BC) or elemental carbon (EC) particles, based on the laser-induced incandescence (LII) technique. In this study, graphite was used as a surrogate of EC. Graphite particles with mass equivalent diameters of 110–200 nm were layered with organic liquids (glycerol and oleic acid) to produce coated graphite with diameters up to 650–800 nm. These were sampled by the SP2 to measure the waveforms (i.e., time development) of the LII and scattering signals. The peak temperature and the peak LII signal of graphite particles were independent of the coating thickness or the coating material to within experimental errors. These results indicate that the mass of EC can be measured by using peak LII signal without interference by the coating conditions. It was also shown that the difference between the times of the scattering and LII peaks can be used as an indicator of coating on EC with thicknesses larger than about 100–200 nm. LII and scattering waveforms were calculated using a newly developed theoretical model that takes into account the physical processes controlling the temperature and evaporation rate of the coated graphite particle in the laser beam. The calculations reproduced the general features of observed waveforms of LII and scattering signals, providing a firm theoretical basis for the interpretation of the SP2 data.
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Cites
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“In Equation (24), Tp and pressure in the SP2 chamber are used as T and Ptotal, respectively. υ is the parameter (without dimensions) for each atom in a molecular constituent (Fuller et al. 1966). υ is 16.5 for C, 1.98 for H, 5.48 for O.”
BackgroundMethodInfluentialStrong radiative heating due to the mixing state of black carbon in atmospheric aerosols
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Cited by
Bounding the role of black carbon in the climate system: A scientific assessment
Bond, T. C., Doherty, S. J., Fahey, D. W., Forster, P. M., Berntsen, T., DeAngelo, B. J., Flanner, M. G., Ghan, S., Kärcher, B., Koch, D., et al. (2013) · Journal of Geophysical Research: Atmospheres · doi:10.1002/jgrd.50171 · Cited by 6,385
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Metadata
- Authors
- Moteki, N., & Kondo, Y.
- Venue
- Aerosol Science and Technology
- Publisher
- Informa UK Limited
- Published
- 2007-03
- Volume
- 41
- Issue
- 4
- Pages
- 398-417
- ISSN
- 0278-6826 (ISSN-L)
- 1521-7388
- OpenAlex
- W2086820438
- Cited by
- 309
- References
- 31
- FWCI
- 6.00
- Type
- journal article
- Language
- en
- Open access
- bronze
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Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.