Concentrations of sulphate in precipitation in southern Norway have decreas
ed by 50-60% from 1980-1999. This has caused a decrease in sulphate concent
rations in lakes of 30-40% from 1986-1999. Nitrogen in precipitation has de
creased slightly over the last 10-years. In lakewater there has also been a
significant but slight decrease. Concentrations of non-marine base cations
in precipitation have decreased by 40% from 1980-1999. In lakewater, non-m
arine base cation concentrations have been at about the same level the last
10 years. This indicates that acid deposition has decreased sufficiently s
uch that the pool of exchangeable base cations in the soil is now being rep
lenished. The acidification situation in lakes in Norway has thus shown a c
lear improvement over the last 8-10 years. pH, alkalinity and ANC (acid neu
tralising capacity) have all increased. Concentrations of inorganic (toxic)
aluminium species have decreased. The trends in H+ and Aln+ do not follow
the relation expected if Aln+ concentrations were governed solely by a sing
le solid phase of Al(OH)(3).