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Can light absorption of black carbon still be enhanced by mixing with absorbing materials? / Feng, Xue; Wang, Jiandong; Teng, Shiwen et al.

In: Atmospheric Environment, Vol. 253, 118358, 15.05.2021.

Research output: Contribution to journalArticlepeer-review

Harvard

Feng, X, Wang, J, Teng, S, Xu, X, Zhu, B, Wang, J, Zhu, X, Yurkin, MA & Liu, C 2021, 'Can light absorption of black carbon still be enhanced by mixing with absorbing materials?', Atmospheric Environment, vol. 253, 118358. https://doi.org/10.1016/j.atmosenv.2021.118358

APA

Feng, X., Wang, J., Teng, S., Xu, X., Zhu, B., Wang, J., Zhu, X., Yurkin, M. A., & Liu, C. (2021). Can light absorption of black carbon still be enhanced by mixing with absorbing materials? Atmospheric Environment, 253, [118358]. https://doi.org/10.1016/j.atmosenv.2021.118358

Vancouver

Feng X, Wang J, Teng S, Xu X, Zhu B, Wang J et al. Can light absorption of black carbon still be enhanced by mixing with absorbing materials? Atmospheric Environment. 2021 May 15;253:118358. doi: 10.1016/j.atmosenv.2021.118358

Author

Feng, Xue ; Wang, Jiandong ; Teng, Shiwen et al. / Can light absorption of black carbon still be enhanced by mixing with absorbing materials?. In: Atmospheric Environment. 2021 ; Vol. 253.

BibTeX

@article{4c6f95ebebb94346939559eeef998671,
title = "Can light absorption of black carbon still be enhanced by mixing with absorbing materials?",
abstract = "Strongly absorbing black carbon (BC) particles are commonly mixed with other aerosols in the ambient atmospheres, resulting in absorption enhancement known as the lensing effect. If other absorbing aerosols such as mineral dust and brown carbons (BrCs) are mixed with BC particles, resulting absorption properties are still less certain. Such mixtures are common due to large amounts of BrC (and tarballs) co-emitted with BC from biomass burning. Thus, this study focuses on mixtures of two absorbing carbonaceous aerosols with different spectral variations of absorption, and reveals the influences of mixing states on their absorption, especially on their spectral variation and enhancement. Three typical mixing states (internally, partially and externally mixed) and complex nonspherical BC structures (fractal aggregates) are considered accurately in the light scattering simulations. The absorption Angstrom exponent (AAE) of internally mixed particles can increase to over 2 when BrC volume fraction is above 70%, but it is systematically smaller (by up to 0.1) than those of the partially mixed and externally mixed particles. Different from non-absorbing coating acting as a lens, internal mixing of BC and BrC may not enhance BC absorption at shorter wavelengths, while the total absorption may even be reduced due to the “protection” of BC by the BrC coating, referred to as a “shielding effect”. Specifically, absorption enhancement in the case of internal mixing is sensitive to coating absorptivity (influenced by both its refractive index and volume fraction), and becomes close to or even smaller than 1 as the coating becomes more absorbing. Furthermore, the mixing states of two absorbing aerosols would surely affect absorption attribution as well as downstream estimations of BC heating effects. Thus, it should be carefully considered in future studies.",
keywords = "Absorbing aerosols, Black carbon, Brown carbon, Light absorption enhancement",
author = "Xue Feng and Jiandong Wang and Shiwen Teng and Xiaofeng Xu and Bin Zhu and Jiaping Wang and Xijuan Zhu and Yurkin, {Maxim A.} and Chao Liu",
note = "Publisher Copyright: {\textcopyright} 2021 Elsevier Ltd",
year = "2021",
month = may,
day = "15",
doi = "10.1016/j.atmosenv.2021.118358",
language = "English",
volume = "253",
journal = "Atmospheric Environment",
issn = "1352-2310",
publisher = "Elsevier Science Publishing Company, Inc.",

}

RIS

TY - JOUR

T1 - Can light absorption of black carbon still be enhanced by mixing with absorbing materials?

AU - Feng, Xue

AU - Wang, Jiandong

AU - Teng, Shiwen

AU - Xu, Xiaofeng

AU - Zhu, Bin

AU - Wang, Jiaping

AU - Zhu, Xijuan

AU - Yurkin, Maxim A.

AU - Liu, Chao

N1 - Publisher Copyright: © 2021 Elsevier Ltd

PY - 2021/5/15

Y1 - 2021/5/15

N2 - Strongly absorbing black carbon (BC) particles are commonly mixed with other aerosols in the ambient atmospheres, resulting in absorption enhancement known as the lensing effect. If other absorbing aerosols such as mineral dust and brown carbons (BrCs) are mixed with BC particles, resulting absorption properties are still less certain. Such mixtures are common due to large amounts of BrC (and tarballs) co-emitted with BC from biomass burning. Thus, this study focuses on mixtures of two absorbing carbonaceous aerosols with different spectral variations of absorption, and reveals the influences of mixing states on their absorption, especially on their spectral variation and enhancement. Three typical mixing states (internally, partially and externally mixed) and complex nonspherical BC structures (fractal aggregates) are considered accurately in the light scattering simulations. The absorption Angstrom exponent (AAE) of internally mixed particles can increase to over 2 when BrC volume fraction is above 70%, but it is systematically smaller (by up to 0.1) than those of the partially mixed and externally mixed particles. Different from non-absorbing coating acting as a lens, internal mixing of BC and BrC may not enhance BC absorption at shorter wavelengths, while the total absorption may even be reduced due to the “protection” of BC by the BrC coating, referred to as a “shielding effect”. Specifically, absorption enhancement in the case of internal mixing is sensitive to coating absorptivity (influenced by both its refractive index and volume fraction), and becomes close to or even smaller than 1 as the coating becomes more absorbing. Furthermore, the mixing states of two absorbing aerosols would surely affect absorption attribution as well as downstream estimations of BC heating effects. Thus, it should be carefully considered in future studies.

AB - Strongly absorbing black carbon (BC) particles are commonly mixed with other aerosols in the ambient atmospheres, resulting in absorption enhancement known as the lensing effect. If other absorbing aerosols such as mineral dust and brown carbons (BrCs) are mixed with BC particles, resulting absorption properties are still less certain. Such mixtures are common due to large amounts of BrC (and tarballs) co-emitted with BC from biomass burning. Thus, this study focuses on mixtures of two absorbing carbonaceous aerosols with different spectral variations of absorption, and reveals the influences of mixing states on their absorption, especially on their spectral variation and enhancement. Three typical mixing states (internally, partially and externally mixed) and complex nonspherical BC structures (fractal aggregates) are considered accurately in the light scattering simulations. The absorption Angstrom exponent (AAE) of internally mixed particles can increase to over 2 when BrC volume fraction is above 70%, but it is systematically smaller (by up to 0.1) than those of the partially mixed and externally mixed particles. Different from non-absorbing coating acting as a lens, internal mixing of BC and BrC may not enhance BC absorption at shorter wavelengths, while the total absorption may even be reduced due to the “protection” of BC by the BrC coating, referred to as a “shielding effect”. Specifically, absorption enhancement in the case of internal mixing is sensitive to coating absorptivity (influenced by both its refractive index and volume fraction), and becomes close to or even smaller than 1 as the coating becomes more absorbing. Furthermore, the mixing states of two absorbing aerosols would surely affect absorption attribution as well as downstream estimations of BC heating effects. Thus, it should be carefully considered in future studies.

KW - Absorbing aerosols

KW - Black carbon

KW - Brown carbon

KW - Light absorption enhancement

UR - http://www.scopus.com/inward/record.url?scp=85103769514&partnerID=8YFLogxK

U2 - 10.1016/j.atmosenv.2021.118358

DO - 10.1016/j.atmosenv.2021.118358

M3 - Article

AN - SCOPUS:85103769514

VL - 253

JO - Atmospheric Environment

JF - Atmospheric Environment

SN - 1352-2310

M1 - 118358

ER -

ID: 28327493