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International Journal of Environmental Research
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Contribution of Soil, Sulfate, and Biomass Burning Sources to the Elemental Composition of PM10 from Mexico City

Article 3, Volume 6, Number 3, Spring 2012, Page 597-612  XML PDF (659 K)
Document Type: Original Research Paper
Authors
1V.A. Barrera; 1J. Miranda ; 1A.A. Espinosa; 1J. Meinguer; 1J.N. Martínez; 1E. Cerón; 2J.R. Morales; 2P.A. Miranda; 3J.F. Dias
1Instituto de Física, Universidad Nacional Autónoma de México, A.P. 20-364, México, D.F., Mexico
2Departamento de Física, Facultad de Ciencias, Universidad de Chile, Las Palmeras 3425, Ñuñoa, Santiago, Chile
3Universidade Federal do Rio Grande do Sul, Porto Alegre, Brazil
Abstract

This study is aimed to identify sources of particulate matter with mean aerodynamic diameter
below 10 μm (PM10) present in the atmosphere of the Metropolitan Area of Mexico City (MAMC), using
samples obtained from January 1st to June 30th, 2009, analyzed with X-ray spectrometric techniques.
MiniVol samplers were used to collect samples on polycarbonate filters in three sites (North, Center, and
South) of the MAMC. The filters were exposed along 24 h every two days, starting at 8:00 AM, and then
analyzed with particle induced X-ray emission (PIXE), a microPIXE (μPIXE) system, and X-ray fluorescence
(XRF). Statistical multivariate tests with positive matrix factorization (PMF) were conducted to identify
possible contributing factors. The model HYSPLIT was used to determine back-trajectories and the MODIS
database for fire spot localization. The multivariate methods identified five factors in the Center and South,
and four in the North, including Soil, Sulfate, Fuel/Industry, and Biomass burning, with certain differences in
the factors and contributions. Application of HYSPLIT back-trajectories associated these factors to three
main Soil sources and points of secondary aerosols production, as well as locations where Biomass burning
aerosols were originated. The combination of X-ray spectrometric methods, receptor modeling, back-trajectory
determination, and fire site localization, allowed the identification of possible sources of PM10 in the MAMC,
namely, the dry Texcoco lake, the Toluca Valley, and the North dry plains for Soil aerosols, the influence of
local industrial areas for Sulfate (secondary) aerosols, and the appearance of fires for Biomass burning.

Keywords
Aerosols; Mexico City; PIXE; μPIXE; XRF; PMF
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