Abstract
The discovery that man-made halogenated gases such as the chlorofluorocarbons have affected the rate of ozone destruction in the upper atmosphere has stimulated a burgeoning interest in identifying and quantifying the natural sources of volatile halogenated compounds. In terms of atmospheric abundance the most important of these compounds are undoubtedly the gaseous monohalomethanes, in particular chloromethane (CH3Cl). However other less volatile polyhalogenated compounds such as bromoform (CHBr3) are also formed in nature in substantial quantities. The mean concentrations of these compounds in the atmosphere and in seawater are given in Table 1 with estimates for each of the annual global inputs to the atmosphere from both natural and anthropogenic sources. An approximate residence time for each compound in the atmosphere is also included. This paper will review current knowledge concerning the natural sources of these halomethanes and the mechanisms by which they are formed. The environmental significance of the amounts produced will be considered.
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Harper, D.B. (1995). The contribution of natural halogenation processes to the atmospheric halomethane burden. In: Grimvall, A., de Leer, E.W.B. (eds) Naturally-Produced Organohalogens. Environment & Chemistry, vol 1. Springer, Dordrecht. https://doi.org/10.1007/978-94-011-0061-8_2
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DOI: https://doi.org/10.1007/978-94-011-0061-8_2
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