The Forest Roof project at Lake Gardsjon located on the Swedish Southwest c
oast near Gothenburg was established to assess the response of the ecosyste
m following a major reduction in loading of sulfur acidic deposition. The o
bjective of the study was to describe the adsorption-desorption processes o
f sulfate in Haplorthod soils at the Gardsjon site. A sequential batch tech
nique was used to sequentially leach the upper three mineral horizons with
forest floor leachate containing different concentrations of sulfate. Resul
ts showed that adsorption-desorption processes were highly irreversible and
hysterestic in nature. Moreover, the soil solution SO42-, pH and DOC were
interrelated. These findings suggest that improvements in the prediction ca
pability of models for acidified surface waters, lakes and soils are needed
. Therefore, existing sulfate models with fully reversible Langmuir or Freu
ndlich approaches need to account for additional ir-reversible reactions.