Abstract

Annual emissions of anthropogenic Hg to the atmosphere in different regions of the world during the last decade show an interesting dichotomy: the emissions in the developed countries increased at the rate of about 4.5–5.5% yr −1 up to 1989 and have since remained nearly constant, while in developing countries the emissions continue to rise steadily at the rate of 2.7–4.5% yr −1. On a global basis, however, the total anthropogenic emissions of Hg increased by about 4% yr −1 during the 1980s, peaked in 1989 at about 2290 t and are currently decreasing at the rate of about 1.3% yr −1. Solid waste disposal through incineration processes is the dominant source of atmospheric mercury in North America (∼ 40%), Central and South America (∼34%), western Europe (∼28%) and Africa (∼30%), whereas coal combustion remains the dominant source in Asia (∼42%) and eastern Europe and the former USSR (∼40%). Mining and smelting of Zn and Pb represent the major industrial source of Hg in Oceania (∼35%).

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