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Autor(en) / Beteiligte
Titel
Brominated Flame Retardants in the Atmosphere of E-Waste and Rural Sites in Southern China: Seasonal Variation, Temperature Dependence, and Gas-Particle Partitioning
Ist Teil von
  • Environmental science & technology, 2011-10, Vol.45 (20), p.8819-8825
Ort / Verlag
Washington, DC: American Chemical Society
Erscheinungsjahr
2011
Quelle
MEDLINE
Beschreibungen/Notizen
  • The recycling of electrical and electronic waste (e-waste) in developing countries has attracted much attention as a significant source of brominated flame retardants (BFRs). Gaseous and particle-bound BFRs were measured in the atmosphere at e-waste and rural sites in southern China during 2007–2008. The annual average concentrations in the air were 3260 ± 3370 and 219 ± 192 pg/m3 for polybrominated diphenyl ethers (PBDEs) and were 546 ± 547 and 165 ± 144 pg/m3 for non-PBDE BFRs at the e-waste and rural sites, respectively. PBDEs had unusually high relative concentrations of di- and tribrominated congeners at the e-waste site. The Clausius–Clapeyron (CC) plots showed that the gaseous concentrations of less brominated BFRs (di- through hexa-BFRs) were strongly controlled by temperature-driven evaporation from contaminated surfaces (e.g., e-waste, soils, and recycled e-waste remains) except for winter. However, weak temperature dependence at the rural site suggests that regional or long-range atmospheric transport was largely responsible for the air concentrations. Gas-particle partitioning (K P) of PBDEs correlated well with the subcooled liquid vapor pressure (P L o) for most sampling events. The varied slopes of log K P versus log P L o plots for the e-waste site (−0.59 to −1.29) indicated an influence of ambient temperature and atmospheric particle properties on the partitioning behavior of BFRs. The flat slopes (−0.23 to −0.80) for the rural site implied an absorption-dominant partitioning. This paper suggests that e-waste recycling in Asian low-latitude regions is a significant source of less brominated BFRs and has important implications for their global transport from warm to colder climates.

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