The effects of acid treatment on soilwater dissolved organic carbon (D
OC) and inorganic chemistry are being monitored at the Humic Lake Acid
ification Experiment (HUMEX) in western Norway. The HUMEX project invo
lves artificial acidification of half of a dystrophic lake and the cor
responding drainage basin. Soil water chemistry data were collected fr
om 30 monitoring lysimeters and 130 grid lysimeters. The samples from
the monitoring lysimeters were collected before and, for a period of t
wo years, after the onset of acid treatment. Operationally-defined fun
ctional fractions of DOC showed that hydrophilic (HPI) and hydrophobic
(HPO) acids account for 60% to 90% of the DOC. In soils rich in DOC,
the HPO acids were dominant, whereas in mineral soil horizons low in D
OC, the HPI acid fractions were highest. The amount of DOC relative to
labile aluminum and iron may determine the HPO/HPI acid ratio. The su
lphate concentration has increased more in the treated than in the ref
erence side. Coincident decreases in DOC and organically complexed alu
minum (Al(o)) concentrations were observed for surface histosol locati
ons. The temporal and spatial variations in c(Al(o)) were mainly expla
ined by variation in c(DOC).