Bo. Berthelsen et E. Steinnes, ACCUMULATION PATTERNS OF HEAVY-METALS IN SOIL PROFILES AS AFFECTED BYFOREST CLEAR-CUTTING, Geoderma, 66(1-2), 1995, pp. 1-14
Vertical distribution of Zn, Pb, Cu and Cd was studied in podzol soil
profiles of adjacent forested and clear-cut areas in a region contamin
ated with Zn, Pb and Cd from long-range atmospheric transport. This wa
s in order to investigate possible effects of deforestation on accumul
ation and distribution patterns of these metals in surface soil profil
es. Lower Zn and Cd contents were observed in the H horizon of clear-c
ut area soils than in forest area soils. However, this was not suffici
ent to entail a significantly lower total Zn and Cd pool in the humus
layer of clear-cut area soils compared to forest area soils. The total
content of Pb in the L + F + H horizons was significantly lower in cl
ear-cut than in forested areas, attributable to distinctly lower Pb co
ntents in the H horizon of clear-cut area soils. This fact combined wi
th significantly thinner humus layers in clear-cut areas compared to f
orested areas, presents evidence for increased losses of Pb from the h
umus layer after clear-cutting. Higher Pb contents in the Ae and B hor
izons of clear-cut area soils than in forest area soils, show that at
least parts of the Pb lost from the H horizon in clear-cut areas were
re-adsorbed or re-precipitated in the Ae and B horizon. As in the case
of Pb, Cu concentrations were higher in the Ae and B horizons of clea
r-cut area soils compared to forest area soils. In the case of Cu, how
ever, this cannot be explained by increased inputs from the humus laye
r following forest clear-cutting, but rather by increased weathering i
n the Ae and B horizons. The high retention of Zn, Cu and Cd in the hu
mus layer of clear-cut areas, compared to that of Pb, is most probably
due to a stronger accumulation of these metals in ectomycorrhizal bio
mass.