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Isotopes as tracers of sources of lead and strontium in aerosols (TSP & PM2.5) in Beijing
Authors:David Widory  Xiande Liu  Shuping Dong
Institution:1. Priority Organization for Innovation and Excellence, Kumamoto University, 2-39-1 Kurokami, Kumamoto 860-8555, Japan;2. Senior Research Fellow Center, Ehime University, 2-5 Bunkyo-cho, Matsuyama 790-8577, Japan;1. Centro de Pesquisas Geocronológicas, Instituto de Geociências, Universidade de São Paulo, Rua dos Lago, 562, São Paulo, SP, Brazil;2. Centro de Estudos Químicos, UNIFIEO, Av. Franz Voegili, 300, Osasco, SP, Brazil;3. Laboratoire Mixte International-Observatoire des changements Environnementaux–LMI-OCE, Institut de Recherche pour le Développement (IRD)/Universidade de Brasilia, Campus Darcy Ribeiro, L2 Norte, Asa Norte, Brasilia 70910-900, Brazil;4. Departamento de Ciências Atmosféricas, Instituto de Astronomia, Geofísica e Ciências Atmosféricas, Universidade de São Paulo, Rua do Matão, 1226, São Paulo, SP, Brazil
Abstract:Even after its being phased out in gasoline in the late 90s, lead (Pb) is still present at relatively high levels in the atmosphere of Beijing, China (0.10–0.18 μg m?3). Its origin is subject to debate as several distinct sources may contribute to the observed pollution levels. This study proposes to constrain the origin(s) of Pb and strontium (Sr) in aerosols, by coupling both Pb and Sr isotope systematics. The characterisation of the main pollution sources (road traffic, smelters, metal refining plants, coal combustion, cement factories, and soil erosion) shows that they can unambiguously be discriminated by the multi-isotope approach (206Pb/204Pb and 87Sr/86Sr). The study of total suspended particulates (TSP) and fine particles (PM2.5) from Beijing and its vicinity indicates that both size fractions are controlled by the same sources. Lead isotopes indicate that metal refining plants are the major source of atmospheric lead, followed by thermal power stations and other coal combustion processes. The role of this latter source is confirmed by the study of strontium isotopes. Occasionally, emissions from cement plants and/or input from soil alteration are isotopically detectable.
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