Refractive Index of Engine‐Emitted Black Carbon and the Influence of Organic Coatings on Optical Properties

Author:

Hu Dawei1ORCID,Alfarra M. Rami123ORCID,Szpek Kate4ORCID,Langridge Justin M.4ORCID,Cotterell Michael I.5ORCID,Flynn Michael J.1,Shao Yunqi1,Voliotis Aristeidis1ORCID,Du Mao16,Liu Dantong7ORCID,Johnson Ben4ORCID,McFiggans Gordon1,Haywood Jim M.48ORCID,Coe Hugh1,Allan James12ORCID

Affiliation:

1. Department of Earth and Environmental Sciences University of Manchester Manchester UK

2. National Centre for Atmospheric Science University of Manchester Manchester UK

3. Now at Qatar Environment and Energy Research Institute Hamad Bin Khalifa University (HBKU) Doha Qatar

4. Met Office Exeter UK

5. School of Chemistry University of Bristol Bristol UK

6. Now at School of Geography Earth and Environment Sciences University of Birmingham Birmingham UK

7. Department of Atmospheric Sciences School of Earth Sciences Zhejiang University Hangzhou China

8. College for Engineering Mathematics and Physical Sciences University of Exeter Exeter UK

Abstract

AbstractRefractive indices (RI) of particles are important in determining their radiative forcing. We measured optical coefficients of particles classified according to their aerodynamic diameter, allowing retrieval of RI using a Mie model. At 405 nm, the RI of BC from a diesel engine was 1.870 (±0.132) + 0.640 (±0.015) i. The RI of secondary organic aerosol (SOA), using α‐pinene and o‐cresol as precursors, were 1.584 ± 0.015 and 1.738 (±0.021) + 0.0316 (±0.0018) i, respectively. Neither SOAs demonstrated absorption at 660 nm and their RIs were 1.551 ± 0.011 and 1.586 ± 0.011, the similar value suggesting that a single RI may be sufficient for simulating the radiative forcing of SOA at this wavelength. In addition, organics were condensed onto BC to test optical models for coated particles. For BC particles coated with non‐absorbing organics, the extinction is predicted accurately by all models. The absorption is significantly over‐estimated by core‐shell, volume mixing, and effective medium approximations and under‐estimated by external mixing. For BC particles coated with weakly absorbing organics, the extinction and absorption are best described by external mixing when the coating ratio is less than 2.5. When the coating ratio is over 2.5, the difference between the external mixing predictions and measurements increases with the coating ratio. Our results show that the absorption of coated BC particles may not be predicted accurately based solely on the equivalent diameter, coating ratio, and pure component RIs, and considerations of additional factors such as morphology may be necessary.

Funder

Natural Environment Research Council

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

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