By Sven-Tage Teodorsson
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Extra resources for Anaxagoras' Theory of Matter (Studia Graeca Et Latina Gothoburgensia)
The forest areas on the Veluwe and the Utrecht Heuvelrug, and in Brabant, Limburg and Overijssel are easily identifiable on the deposition maps. The most deposition is found in areas of great roughness (forests, towns) close to sources. In 1993 the highest mean load (to a 5x5 km 2 area) of SO~ was 3815 mol haly 1 and that of NOy was 1285 mol ha~y-1, both in the Rijnmond district. For NH x the highest value was 5185 mol ha~y -~, in North Brabant. The lowest values for SOx, NOy,and NH x were 235, 380 and 465 mol ha-~y~, respectively.
I 930 1000 980 690 710 dry 1340 1660 1580 1410 830 NHx i wet 740 770 760 800 630 tot. 2080 2430 2340 2210 1460 dry 1950 2350 2240 1780 1230 wet 1060 1100 1080 1120 950 tot. 3010 3450 3320 2900 2180 3420 3980 3820 2620 2270 wet i 1490 1540 1500 1560 1300 tot. i 4910 5520 5320 4180 3570 dry I SOx NOy N i dry ! 2 for 2000 and 2010 and the OPS model. The calculation was performed with the spatial distribution of the emissions in 1990. 11 shows the calculated spatial distribution for the deposition of total potential acid in 2000 and 2010.
The deposition will be under the target level in only a small part of the country. 11 total potentialacid deposition in 2010 in mol/ha/y .. < 1400 1400-1900 19oo-24oo S ,,~ ~ 2400-2900 > 2900 The spatial distribution of the total potential acid deposition in 2000 and 2010 (mol haLyt). 3 L - The spatial distribution of the total nitrogen deposition in 2000 and 2010 (mol Deposition ha~y~). o f b a s e c a t i o n s in T h e N e t h e r l a n d s The information acquired by the "Aerosol Project" has permitted local estimates of base cation deposition in The Netherlands to be made for the first time.