The present study focused on the estimation of the personal dose of airborne particles using an exposure dose model (ExDoM2). Input data from three European cities (Athens, Kuopio, Lisbon) were selected to implement the model that calculates the deposited dose and retention of particles in the respiratory tract, the mass transferred to the oesophagus and the absorption to blood as well as the dose for five particle-bound metals. Model results showed that after one day exposure higher deposited dose in the respiratory tract was obtained for Lisbon as a direct consequence of the higher PM concentration measured in this city. Moreover, the activity profile and the physical characteristics of the exposed subject had strong impact on the estimated deposited dose. Thus, light activity corresponded to higher deposited dose compared to no activity as well as an adult male exhibited higher dose, both findings associated with increased inhalation rate. Regarding the internal dose for particle-bound metals higher dose for four out of the five metals was obtained in lungs followed by the muscles for As, the gastrointestinal tract for Cr, the other tissues for Mn, the intestines for Cd and finally for Pb higher dose was found in bones and blood.
Abstract. Aerosol particles are essential constituents of the Earth's atmosphere, impacting the earth radiation balance directly by scattering and
absorbing solar radiation, and indirectly by acting as cloud condensation
nuclei. In contrast to most greenhouse gases, aerosol particles have short
atmospheric residence times, resulting in a highly heterogeneous distribution in space and time. There is a clear need to document this variability at
regional scale through observations involving, in particular, the in situ
near-surface segment of the atmospheric observation system. This paper will provide the widest effort so far to document variability of climate-relevant
in situ aerosol properties (namely wavelength dependent particle light
scattering and absorption coefficients, particle number concentration and
particle number size distribution) from all sites connected to the Global
Atmosphere Watch network. High-quality data from almost 90 stations worldwide have been collected and controlled for quality and are reported
for a reference year in 2017, providing a very extended and robust view of
the variability of these variables worldwide. The range of variability
observed worldwide for light scattering and absorption coefficients, single-scattering albedo, and particle number concentration are presented together with preliminary information on their long-term trends and comparison with
model simulation for the different stations. The scope of the present paper
is also to provide the necessary suite of information, including data provision procedures, quality control and analysis, data policy, and usage of
the ground-based aerosol measurement network. It delivers to users of the World Data Centre on Aerosol, the required confidence in data products in
the form of a fully characterized value chain, including uncertainty estimation and requirements for contributing to the global climate
monitoring system.
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