The atmosphere in Europe is polluted by easily available nitrogen (amm
onium and nitrate) mainly from livestock (NH3), traffic (NOx) and stat
ionary combustion sources (NOx). The nitrogen emission from various Eu
ropean sources decreases in the order: agriculture, road traffic, stat
ionary sources and other mobile sources (including vehicular emissions
from agriculture), with annual emissions of approximately 4.9, 2.7, 2
.7 and 0.8 Mt N respec tively. The emissions have increased dramatical
ly during the latest decades. In the atmosphere the pollutants are oxi
dised to more water soluble compounds that are washed out by clouds an
d eventually brought back to the earth's surface again. Since ammonia
is emitted in a highly water soluble form it will also to a substantia
l degree be dry deposited near the source. Ammonia is, however, the do
minant basic compound in the atmosphere and will form salts with acidi
c gases. These salt particles can be transported long distances especi
ally in the absence of clouds. The deposition close to the source is s
ubstantial, but hard to estimate due to interaction with other polluta
nts. Far from the source the deposition of ammonium is on an annual av
erage halved approximately every 400 km. This short transport distance
and the substantial deposition near the source makes it possible for
countries to control their ammonium deposition by decreasing their emi
ssions, provided that there is no country with much higher emission in
the direction of the prevailing wind trajectory. When the easily avai
lable nitrogen is deposited on natural ecosystems (lakes, forests), ne
gative effect can occur. The effect is determined by the magnitude of
the deposition and the type of ecosystems (its critical load for nitro
gen). In order to reduce the negative effects by controlling the emiss
ions in a cost-efficient way it Is necessary to use atmospheric transp
ort models and critical loads.