S. Piirainen et al., Deposition and leaching of sulphate and base cations in a mixed boreal forest in eastern Finland, WATER A S P, 133(1-4), 2002, pp. 185-204
Monthly fluxes of sulphate (SO42-) and base cations (Ca2+, Mg2+, K+) were s
tudied from 1993 to 1996 as precipitation passed through forest vegetation
and surface soil layers in an area receiving low and declining levels of at
mospheric sulphate pollution. The canopy was dominated by mature Norway spr
uce (Picea abies Karsten) and the soil was a podzol developed on glacial ti
ll material. The mean annual bulk deposition of SO42- collected in the open
was 136 mol(c) ha(-1) and that of Ca2+, Mg2+ and K+ was 44, 11 and 25 mol(
c) ha(-1), respectively. The annual total throughfall deposition of SO42- w
as 318 mol(c) ha(-1) and that of Ca2+, Mg2+ and K+ was 151, 64 and 181 mol(
c) ha(-1), respectively. Sulphate was the dominant anion accompanying the b
ase cations leached from the canopy. More than half (58%) of the annual tot
al throughfall deposition of SO42- was retained by the O-horizon and only 1
5% leached from below the B-horizon. The annual leaching of Ca2+, Mg2+ and
K+ from below the B-horizon was 14, 25 and 9% of the annual total throughfa
ll deposition, respectively. The transport of base cations through the soil
was predominantely countered by SO42- anions.