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Atmospheric Environment
journal homepage: www.elsevier.com/locate/atmosenv
Thermo-optical properties of residential coals and combustion aerosols
Máté Pintér
a
, Tibor Ajtai
a,b,c,*
, Gergely Kiss-Albert
a,d
, Noémi Utry
b
, Diána Kiss
a
, Tomi Smausz
a,b
,
Attila Kohut
a
, Béla Hopp
a
, Gábor Galbács
e
, Ákos Kukovecz
f,g
, Zoltán Kónya
f,g
, Gábor Szabó
a,b
,
Zoltán Bozóki
a,b
a
Department of Optics and Quantum Electronics, University of Szeged, H-6720 Szeged, Hungary
b
MTA-SZTE Research Group on Photoacoustic Spectroscopy, H-6720 Szeged, Hungary
c
ELI-HU Non-Profit Ltd., H-6720 Szeged, Hungary
d
Hilase Development, Production, Service and Trading Limited, Székesfehérvár H-8000, Hungary
e
Department of Inorganic and Analytical Chemistry, University of Szeged, Dom Square 7, 6720 Szeged, Hungary
f
Department of Applied and Environmental Chemistry, University of Szeged, Szeged, Rerrich Béla tér 1, 6720, Hungary
g
MTA-SZTE Reaction Kinetics and Surface Chemistry Research Group, Szeged, Rerrich Béla tér 1, 6720, Hungary
ARTICLE INFO
Keywords:
PhotoAcoustic Spectroscopy
Household coal
Laser ablation
Aerosol Angström Exponent
Calorific value
ABSTRACT
In this study, we present the inherent optical properties of carbonaceous aerosols generated from various coals
(hard through bituminous to lignite) and their correlation with the thermochemical and energetic properties of
the bulk coal samples. The nanoablation method provided a unique opportunity for the comprehensive in-
vestigation of the generated particles under well controlled laboratory circumstances. First, the wavelength
dependent radiative features (optical absorption and scattering) and the size distribution (SD) of the generated
particulate matter were measured in-situ in aerosol phase using in-house developed and customised state-of-the-
art instrumentation. We also investigated the morphology and microstructure of the generated particles using
Transmission Electron Microscopy (TEM) and Electron Diffraction (ED). The absorption spectra of the measured
samples (quantified by Absorption Angström Exponent (AAE)) were observed to be distinctive. The correlation
between the thermochemical features of bulk coal samples (fixed carbon (FC) to volatile matter (VM) ratio and
calorific value (CV)) and the AAE of aerosol assembly were found to be (r
2
= 0.97 and r
2
= 0.97) respectively.
Lignite was off the fitted curves in both cases most probably due to its high optically inactive volatile material
content. Although more samples are necessary to be investigated to draw statistically relevant conclusion, the
revealed correlation between CV and Single Scattering Albedo (SSA) implies that climatic impact of coal com-
busted aerosol could depend on the thermal and energetic properties of the bulk material.
1. Introduction
Atmospheric carbonaceous particulate matter (CPM) is in the focus
of scientific interest due its adverse climatic and human health effects (;
Andreae and Ramanathan, 2013; Stocker et al., 2013; Penner et al.,
1992; Yu et al., 2006; Pope and Dockery, 1996). Ambient aerosol
particles emitted from fossil fuel combustion alter the energy budget of
the Earth-atmosphere system through scattering and absorbing solar
radiation (Bond et al., 2013). Particles that do not absorb, only scatter
solar light (e.g. sulfates) produce a cooling effect (Charlson et al.,
1991). However, aerosol particles with significant optical absorption in
the solar wavelength range cause a remarkable heating effect
(Haywood and Shine, 1995). Black Carbon (BC) is the most dominant
component of atmospheric light absorbing carbonaceous particulate
matter (LAC) (Bond et al., 2013; Rosen et al., 1981). Today, the
radiative forcing of BC is one of the biggest uncertainties in climatic
models (Bond et al., 2013; Lack et al., 2006). The most important
reasons for that are found in the lack of proper knowledge regarding
CPM emission rates, lifetimes and optical properties (Bond et al., 2002).
Climatic models require the precise and reliable determination of size
distribution and the complex optical properties of CPM as input para-
meters (Bond et al., 2002; Twomey, 1977).
Due to their availability and low price, coal alongside with biofuels
have gained new popularity in developing and developed countries as
well (Khodaei et al., 2017; Weldu et al., 2017). Carbonaceous particles
emitted from domestic coal combustion for both cooking and heating
make a significant contribution to the atmospheric concentration of
particulate matter (PM) a global and a regional scale as well (Cooke
et al., 1999; Bond et al., 2002). According to the most recent estima-
tions, coal burning contributes to almost 50% of CPM emitted from
https://doi.org/10.1016/j.atmosenv.2018.01.036
Received 24 August 2017; Received in revised form 20 December 2017; Accepted 23 January 2018
*
Corresponding author. Department of Optics and Quantum Electronics, University of Szeged, H-6720 Szeged, Hungary.
E-mail address: ajtai@titan.physx.u-szeged.hu (T. Ajtai).
Atmospheric Environment 178 (2018) 118–128
1352-2310/ © 2018 Published by Elsevier Ltd.
T