A source-specific, spatially resolved mercury emission inventory is a key i
nput to an air-quality model that is used to understand relationships betwe
en mercury emissions and observed deposition. Previously we simulated the t
ransport and deposition of anthropogenic mercury emissions in the contiguou
s United States. Due to the long residence time of elemental mercury, i.e.,
1 year, it is possible that mercury deposition observed at receptors in th
e US could be due to long-range transport of emissions across political bou
ndaries. We have recently added mercury emission estimates of anthropogenic
sources in Canada and Mexico, to our US inventory. This combined inventory
will be used with a regional model to understand source-receptor relations
hips of atmospheric mercury emissions in North America. Our estimate of 272
Mg of mercury emissions from various anthropogenic sources in North Americ
a is comparable to estimates in global inventories (ranging from 240 to 333
Mg). In this paper we discuss the differences in the three regional invent
ories, i.e., US, Canada, and Mexico, for the year 1990. The dominant source
categories of mercury emissions in 1990 in the three regions are different
. While combustion of municipal waste and coal accounts for 56% of the 176
Mg mercury emissions in the US in 1990, smelting of nonferrous metals repre
sents the largest source of mercury emissions in Canada (= 24 Mg) and Mexic
o (= 31 Mg) in 1990. The main source of uncertainty in the emission estimat
es is due to the emission factors used in estimation. The emission factors
are derived from measurements at a limited number of sources and could pote
ntially not be representative of the operating conditions at other sources
for which they are used. In addition, the inventories could still be missin
g potentially important source categories due to lack of data to develop re
liable emission factors. These sources of uncertainties are common features
of all three inventories and clearly point to additional research needs. (
C) 2000 Elsevier Science B.V. All rights reserved.