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Air Quality Guidelines - World Health Organization Regional Office ...

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introduction<br />

chapter 13<br />

Indirect effects of acidifying<br />

compounds on natural<br />

systems: critical loads<br />

ACIDIFYING DEPOSITION<br />

AND ECOSYSTEM DAMAGE<br />

2– Historical data provide evidence of increasing transport of sulfate (SO4 ),<br />

up to a factor of 2 and 3.5 in 1950 and 1980, respectively, compared to preindustrial<br />

levels in Europe. Emissions of sulfur dioxide in the air are transformed<br />

to sulfate, which constitutes the major compound of acid deposition<br />

(1, 2). The effects and risks of sulfur dioxide emissions and resulting deposition<br />

are described for soils in general and for forest soils and surface waters<br />

in particular.<br />

Soil acidification is defined as a decrease in the acid neutralizing capacity<br />

(ANC) of the inorganic fraction of the soil including the solution phase,<br />

and is directly dependent on the net supply of base cations (by weathering<br />

and deposition) and the net supply of anions (deposition minus retention)<br />

in the mineral soil (3, 4). Deposition of acidifying compounds such as<br />

sulfur dioxide, nitrogen oxides and ammonia leads to soil acidification by<br />

oxidation to sulfuric and nitric acids and leaching of sulfate and nitrate,<br />

respectively.<br />

The dynamics of forest soil acidification is very site-specific and depends on<br />

soil characteristics such as weathering rate, sulfate adsorption capacity and<br />

cation exchange capacity. The acidification of soils ultimately leads to an<br />

increase in the soil solution of the aluminium concentration, which increases<br />

the risk of vegetation damage. By defining the relationship between<br />

the chemical status (base cation and aluminium concentrations in the soil<br />

solution) and vegetation response, the so-called critical load for that particular<br />

ecosystem can be derived (5). Damage to forests in Europe, including<br />

defoliation, discoloration, growth decrease and tree dieback, have been<br />

reported over the last decade, and have to a large extent been attributed to<br />

soil acidification, but also to eutrophication and photochemical oxidant<br />

effects.<br />

– 239 –

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