W. Devries et al., ASSESSMENT OF CRITICAL LOADS AND THEIR EXCEEDANCE ON DUTCH FORESTS USING A MULTILAYER STEADY-STATE MODEL, Water, air and soil pollution, 76(3-4), 1994, pp. 407-448
Critical acid loads for Dutch forests were derived using a multi-layer
steady-state model that includes canopy interactions, nutrient cyclin
g, mineral weathering and N transformations. Values were calculated fo
r combinations of 12 tree species and 23 soil types for a 10 x 10 km g
rid. Critical acid loads thus derived increased with decreasing soil d
epth. Nearly 90% of the values varied approximately between 1500 and 4
000 mol(c) ha-1 yr-1 at 10 cm soil depth and between 750 and 2000 mol(
c) ha-1 yr-1 at the bottom of the rootzone. Separate critical loads ca
lculated for N and S at the bottom of the rootzone varied between appr
oximately 300 and 1000 mol(c) ha-1 yr-1 for N and between 150 and 1250
mol(c) ha-1 yr-1 for S. Using deposition data of 1990, a median reduc
tion of the deposition by approximately 75% was calculated to achieve
the critical loads at the bottom of the rootzone. The overall uncertai
nty in this value was estimated to be about 10%, although it can be mu
ch larger for specific soil types such as clay and peat soils. For N a
larger reduction deposition percentage was calculated than for S, esp
ecially for coniferous forests with a high present N input.