J. Derome et Aj. Lindroos, COPPER AND NICKEL MOBILITY IN PODZOLIC FOREST SOILS SUBJECTED TO HEAVY-METAL AND SULFUR DEPOSITION IN WESTERN FINLAND, Chemosphere, 36(4-5), 1998, pp. 1131-1136
The distribution of copper and nickel down the soil profile has been i
nvestigated at 4 plots along a heavy metal and sulphur gradient extend
ing for a distance of up to 8 km from a copper smelter in Western Finl
and. Emissions from the smelter have earlier been at a relatively high
level, but were considerably reduced at the beginning of the 1990's p
rior to the start of the experiment. Soil samples were taken in 1991,
and soil water quality has been monitored using zero-tension lysimeter
s (5, 20 and 40 cm depth) during the growing season in 1992-1994. The
organic layer and mineral soil on the plot nearest to the smelter cont
ains considerable amounts of Cu and Ni. The Cu/Ni ratio in the organic
layer was much higher than that in the underlying mineral soil, indic
ating that Cu is more strongly adsorbed in the organic layer than Ni.
Copper concentrations in percolation water showed a peak at 20 cm dept
h, while for Ni the concentrations at 40 cm were higher than those at
5 cm. The lower Cu and Ni concentrations at 5 cm depth could be signs
of a gradual detoxification of the surface soil, i.e. the gradual leac
hing of the mobile Cu and Ni components down to greater depths. (C) 19
98 Elsevier Science Ltd.