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Leaching from Organic Matter–Rich Soils by Rain of Different Qualities

I. Concentrations

Agricultural University of Norway, Department of Soil and Water Sciences, P.O. Box 5028, N-1430 Ås, Norway

View larger version (14K): [in a new window]   Fig. 1. Map of Norway showing the site where the soil was collected.

View larger version (36K): [in a new window]   Fig. 2. Concentrations of dissolved organic carbon (DOC) (µM) for lysimeters from both sites shown as mean of two replicates: Heather "normal rain," • Heather "acid rain," Moorgrass "normal rain," Moorgrass "acid rain," F = frost, D = drought.

View larger version (21K): [in a new window]   Fig. 3. Concentrations of SO2-4 (µM) for the Storgama lysimeters shown as mean of two replicates: Heather "normal rain," • Heather "acid rain," Moorgrass "normal rain," Moorgrass "acid rain," F = frost, D = drought.

View larger version (21K): [in a new window]   Fig. 4. Concentrations of NO-3 (µM) for the first two years for the Storgama lysimeters shown as mean of two replicates: Heather "normal rain," • Heather "acid rain," Moorgrass "normal rain," Moorgrass "acid rain," F = frost, D = drought.

View larger version (29K): [in a new window]   Fig. 5. pH variations for lysimeters from both sites shown as mean of two replicates: Heather "normal rain," • Heather "acid rain," Moorgrass "normal rain," Moorgrass "acid rain," F = frost, D = drought.