Hexachlorocyclohexanes in the North American Atmosphere

Li Shen, Frank Wania,* Ying D. Lei, Camilla Teixeira, Derek C. G. Muir, and Terry F. Bidleman§
Department of Chemistry and Department of Physical and Environmental Sciences, University of Toronto at Scarborough, 1265 Military Trail, Toronto, Ontario, Canada M1C 1A4, National Water Research Institute, 867 Lakeshore Road, Burlington, Ontario, Canada L7R 4A6, and Centre for Atmospheric Research Experiments, Meteorological Service of Canada, 6248 Eighth Line, Egbert, Ontario, Canada L0L 1N0
Environ. Sci. Technol., 2004, 38 (4), pp 965–975
DOI: 10.1021/es034998k
Publication Date (Web): January 7, 2004
Copyright © 2004 American Chemical Society

 University of Toronto at Scarborough.

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*

 Corresponding author phone:  (416)287-7225; fax:  (416)287-7279; e-mail:  frank.wania@utoronto.ca.

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 National Water Research Institute.

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§

 Meteorological Service of Canada.

Abstract

Annually integrated air concentrations of α- and γ-hexachlorocyclohexane (HCH) were determined in 2000/2001 at 40 stations across North America using XAD-based passive air samplers to understand atmospheric distribution processes on a continental scale. Elevated levels of γ-HCH in the atmosphere of the Canadian Prairies are consistent with the ongoing use of lindane as a seed treatment on canola and confirm the feasibility of detecting the agricultural use of a pesticide using long-term integrated passive air sampling. In contrast to γ-HCH, the atmospheric concentrations of α-HCH show a rather uniform distribution across Canada and the United States, which is expected for a chemical with no current use on the continent. Higher levels in the atmosphere over Atlantic Canada can be explained by α-HCH evaporating from the waters of the Labrador Current, which is supported by the chiral composition of α-HCH and the temperature dependence of its atmospheric concentrations along the east coast of Canada. Similarly, α-HCH is volatilizing from Lake Superior. Atmospheric HCH levels increase with elevation in the Canadian Rocky Mountains. The results suggest that evaporation, in particular from cold water bodies, is an important source of α-HCH to the North American atmosphere. Low levels of HCHs in Central America hint at efficient degradation under tropical conditions. Chiral analysis shows that (+)-α-HCH is often enriched in air over continental areas and at the Pacific Coast, which is opposite to the enantiomeric enrichment in the proximity to the Great Lakes and the Atlantic Ocean. Passive air sampling is a powerful tool to discern the large-scale variability of semivolatile and persistent organic chemicals in the atmosphere.

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History

  • Published In Issue February 15, 2004
  • Received for review September 11, 2003
    Revised manuscript received November 21, 2003
    Accepted December 2, 2003

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