Аннотация:Since inhalation is dependent on particle size,
atmospheric particulate matter (PM) fractions as well as
detailed size-fractionated characterization of inorganic
particles in PM is of great interest (Eleftheriadis et al.,
2014). In this respect, megacities such as Moscow with
over ten million inhabitants require a special focus. We
present the results of the ongoing investigations aiming
at an in-depth characterization of Moscow PM, based
on the determination of trace elements (TE) and ionic
fraction profiles both in PM10 and in size-segregated
aerosol samples. As a northern latitude megacity, this
type of investigation is expected to fill fundamental
gaps in the understanding of atmospheric dynamics in
such a peculiar urban landscape, wherein systematic
and up-to-date studies, started to be implemented.
Two sampling campaigns have been performed
at the Aerosol Complex of Moscow State University at
southwest of Moscow, classified as urban background
site, the first one from April 2018 to December 2019,
and the second one from September 2021 to August
2022. PM filters have been collected with a MOUDI
impactor, then analyzed by ion chromatography (IC),
proton-induced X-ray emission (PIXE), scanning electron
microscopy (SEM), and energy dispersive X-ray
spectroscopy (EDX). All these methods are well-suited
to size-resolved elemental and ionic speciation of
atmospheric aerosols. Correlations between TE and ions
were evaluated, in conjunction with meteorological
data, and chemometric analyses were carried out to
shed light at a higher degree of detail on aerosol
sources, environmental fate and health hazards in
Moscow megacity airshed.
First results on ionic fraction (Zappi et al. 2023)
evidenced a strong seasonality of pollution, mainly due
to the peculiar climate of that area, characterized by
snowfall starting early in October and that go on until
March. Massive contribution of measured species to
PM10 for each season is shown in Fig.1. Total inorganic
ions (TII) constitute the largest fraction of aerosol mass
in the cold period reaching a maximum of 27% in
autumn, and a minimum of 16.5% in summer. Sulfates
and nitrates dominate among the major anion
components, with maximum contribution of 38 and 34%
to TII in autumn. Cations are mainly represented by
calcium and ammonium. Ca2+ had a maximum of 21% in
spring and minimum of 5% in autumn. Ca2+ and Mg2+
relate to local soil resuspension after snow thaw, Ca2+
shows an additional source from intensive building
activities in the New Moscow area. Seasonality of NH4
+
was not prominent, being 15-17% in any season. A
lower, though significant, fraction of inorganic ions in TII
was represented by sodium and chloride; in summer the
percentage of both Cl- and Na+ approached their
maxima respectively of 5 and 11%, probably due to
resuspension of technical salt used for road
management during snowing periods (confirmations are
expected from TE and EDX analysis), dropping to
minima of 1.6 and 2% in autumn, respectively. Finally,
maximum of K+ fraction of 3% was observed in spring
and autumn. Main sources of PM10 inorganic ions are
secondary sulfates and nitrates, soil resuspension, road
salt, and biomass burning in spring and autumn