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

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indirect effects of acidifying compounds<br />

Table 34. Critical load ranges of acidity used for the various combinations<br />

of parent material and texture in terrestrial ecosystems<br />

Guideline range of Parent material � Texture �<br />

critical loads of acidity<br />

(eq/ha per year)<br />

< 250 acidic coarse<br />

250–500 acidic coarse-medium<br />

intermediate coarse<br />

basic coarse<br />

500–1000 acidic medium, medium-fine<br />

intermediate coarse-medium, medium<br />

basic coarse-medium<br />

1000–1500 intermediate medium-fine<br />

basic medium<br />

> 1500 intermediate fine<br />

basic medium-fine<br />

a Acidic: sand (stone), gravel, granite, quartzine, gneiss (schist, shale, greywacke, glacial till).<br />

Intermediate: gronodiorite, loess, fluvial and marine sediment (schist, shale, greywacke, glacial till).<br />

Basic: gabbro, basalt, dolomite, volcanic deposits.<br />

b Coarse: clay content < 18%.<br />

Medium: clay content 18–35%.<br />

Fine: clay content > 35%.<br />

243<br />

Table 35 lists the ranges of critical loads in relation to combinations of base<br />

cation concentration and runoff classes. For each critical load class, at least<br />

50% of the critical load values computed on the basis of lake data from<br />

Finland (1450 lakes), Norway and Sweden fall within the class boundaries,<br />

given the ranges for present base cation concentrations and runoff. Only in<br />

two cases did the boundaries for the base cation concentration classes overlap<br />

between two critical load classes, when the class boundaries were set on<br />

the basis of the 25 th and 75 th percentile base cation concentrations for given<br />

runoff classes. For those cases the critical loads are determined more by<br />

other factors than base cation levels and runoff, and the guideline value set is<br />

therefore more uncertain than those without overlap.

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