Optical properties of PM2.5 particles: Results from a monitoring campaign in southeastern Italy

被引:36
作者
Romano, Salvatore [1 ]
Perrone, Maria Rita [1 ]
Pavese, Giulia [2 ]
Esposito, Francesco [3 ]
Calvello, Mariarosaria [2 ]
机构
[1] Univ Salento, Dipartimento Matemat & Fis, Lecce, Italy
[2] CNR, Ist Metodol Anal Ambientale, Potenza, Italy
[3] Univ Basilicata, Scuola Ingn, Potenza, Italy
关键词
Intensive optical parameters; Extensive optical parameters; PM2.5; particles; Graphical frameworks; Particle identification methodology; AEROSOL LIGHT-SCATTERING; URBAN COASTAL SITE; BLACK CARBON; BROWN CARBON; ABSORPTION PROPERTIES; SAHARAN DUST; INTERCONTINENTAL TRANSPORT; ANTHROPOGENIC SULFATE; WAVELENGTH DEPENDENCE; ATMOSPHERIC AEROSOLS;
D O I
10.1016/j.atmosenv.2019.01.037
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The performance of aerosol classification schemes based on intensive optical parameters and applied to mixed particle populations monitored at the surface has been investigated to test the ability of optical parameters to identify different types of particles/particle mixtures and explore their complex features. The results show that the combination of two intensive optical parameters does not allow for the unique identification of different particle types. The classification scheme based on the Absorption Angstrom Exponent (AAE) as a function of the Scattering Angstrom Exponent (SAE) and color-coded by the Single Scattering Albedo difference (dSSA) is a good graphical framework to discriminate between different types of particle/particle mixtures. This aerosol classification scheme has been applied to study the optical properties of heterogeneous PM2.5 particles that were monitored at a coastal site of the Central Mediterranean and were significantly affected by both natural and anthropogenic sources also because of long-range transport from surrounding countries. The calculated AAE, SAE, and dSSA hourly means smoothly and continuously vary within their respective range (0.6-3.4, -0.7-3.0, and -0.33-0.52, respectively) because of the different mixing degree of different types of particles. Consequently, the main features of the particle populations depend on the range of the AAE, SAE, and dSSA values. Eight different clusters have been selected within the used graphical framework to identify four key particle populations (dust, marine, OC-dominated, and BC-dominated particles) and four particle mixtures dominated by key aerosol populations. In addition, their main features have been characterized. Particle mixtures consisting of large and low-absorbing particles (LLAP), small and high-absorbing particles (SHAP), dominated by dust, and large organic particles have been characterized. Marine, LLAP, and mixed dust clusters with a SAE value below 1 are responsible for aerosol scattering coefficients (sigma(s); at 470 nm) below 100 Mm(-1). Conversely, SHAP, BC-dominated, and OC-based mixtures are responsible for the highest sigma(s) values and represent dominant particles species.
引用
收藏
页码:35 / 47
页数:13
相关论文
共 99 条
[1]   Measurements of optical properties of atmospheric aerosols in Northern Finland [J].
Aaltonen, V ;
Lihavainen, H ;
Kerminen, VM ;
Komppula, M ;
Hatakka, J ;
Eneroth, K ;
Kulmala, M ;
Viisanen, Y .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2006, 6 :1155-1164
[2]   ABSORPTION OF VISIBLE RADIATION IN ATMOSPHERE CONTAINING MIXTURES OF ABSORBING AND NON-ABSORBING PARTICLES [J].
ACKERMAN, TP ;
TOON, OB .
APPLIED OPTICS, 1981, 20 (20) :3661-3668
[3]   Black carbon or brown carbon?: The nature of light-absorbing carbonaceous aerosols [J].
Andreae, M. O. ;
Gelencser, A. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2006, 6 :3131-3148
[4]  
[Anonymous], 2016, ARXIV
[5]  
[Anonymous], 1984, AGU GEOPHYS MONOGR S
[6]  
[Anonymous], 2015, ACTRIS 2 WP3 WORKSH
[7]  
[Anonymous], 2015, Light Scattering Reviews 9: Light Scattering and Radiative Transfer, DOI [DOI 10.1007/978-3-642-37985-71, 10.1007/978-3-642-37985-7_1]
[8]   Towards aerosol light-absorption measurements with a 7-wavelength Aethalometer:: Evaluation with a photoacoustic instrument and 3-wavelength nephelometer [J].
Arnott, WP ;
Hamasha, K ;
Moosmüller, H ;
Sheridan, PJ ;
Ogren, JA .
AEROSOL SCIENCE AND TECHNOLOGY, 2005, 39 (01) :17-29
[9]   Solar absorption by elemental and brown carbon determined from spectral observations [J].
Bahadur, Ranjit ;
Praveen, Puppala S. ;
Xu, Yangyang ;
Ramanathan, V. .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2012, 109 (43) :17366-17371
[10]   Aerosol characterization in Northern Africa, Northeastern Atlantic, Mediterranean Basin and Middle East from direct-sun AERONET observations [J].
Basart, S. ;
Perez, C. ;
Cuevas, E. ;
Baldasano, J. M. ;
Gobbi, G. P. .
ATMOSPHERIC CHEMISTRY AND PHYSICS, 2009, 9 (21) :8265-8282