『Abstract
Santiago de Chile is a big city with huge air quality problems,
being one of the most polluted cities in the world. This is aggravated
during winter by the topography and meteorological conditions
of the city. Although public policies have been developed to minimise
the atmospheric aerosol pollution, there is a lack of adequate
knowledge and poor characterisation of these aerosols (in its
PM2.5 and PM10 fractions).
In this study we sampled atmospheric particles during winter in
two distinct areas of Santiago: downtown (Teatinos Street) and
in a more residential area (Macul). Major (Si, Al, Fe, Ca and
K) and some trace element (S, Cl, Ti, P, Cr, Cu and Zn) compositions
were obtained by proton-induced X-ray emission (PIXE). Morphological,
type and chemical characterisation was also performed using scanning
electron microscopy (SEM) coupled with an energy dispersive X-ray
microanalysis system (SEM-EDX). Besides the carbon particles,
the contribution of which can be quite important in the atmospheric
aerosol, especially in downtown, unambiguously lithogenic (i.e.
of geological origin) particles and elements are the second highest
contributors. Enrichment factor calculation, together with particle
identification and element correlation allow the origin of some
elements and particles to be traced, revealing anthropogenic origins
for some of them that are specific to the Santiago area.
Keywords: Atmospheric aerosol; Particle analysis; Mineralogy;
Geochemistry; Environmental pollution』
Introduction
Geographical meteorological and geological context
Sampling and analytical techniques
Results
Gravimetric data
PIXE data
SEM data
1. Nature of the particles and their distribution in both sites:
site effect
(a) Geological particles
(b) Other particles
2. The nature and distribution of the particles between PM10 and PM2.5 fractions (Macul):
size effect
3. The nature and distribution of the particles in relation to
the date (meteorological conditions)
Discussion
Samples of the particles
Sources for the geological particles
Origin of Fe oxides
Origin of CaCO3 and CaSO4
particles
Sources of the different anthropogenic particles
Conclusions
Acknowledgments
References