The long-term effects of catchment liming and reduced sulphur deposition on forest soils and runoff chemistry in southwest Sweden

• Published in: Forest ecology and management 2009-08, Vol.258 (5), p.567-578
• Main Authors: Löfgren, Stefan, Cory, Neil, Zetterberg, Therese, Larsson, Per-Erik, Kronnäs, Veronika
• Format: Article
• Language: English
• Subjects: Acidification; Agronomy. Soil science and plant productions; Animal and plant ecology; Animal, plant and microbial ecology; atmospheric deposition; Biological and medical sciences; Environmental Sciences; Forest liming; Forest Science; forest soils; forested watersheds; Forestry; Fundamental and applied biological sciences. Psychology; General agronomy. Plant production; Geochemistry; Geokemi; hydrochemistry; Liming; Miljövetenskap; Other nutrients. Amendments. Solid and liquid wastes. Sludges and slurries; runoff; simulation models; Skogsvetenskap; Soil; soil acidification; soil chemical properties; soil organic matter; Soil-plant relationships. Soil fertility. Fertilization. Amendments; streams; sulfur; Synecology; Terrestrial ecosystems; Water; water quality; watershed management; watersheds; Whole catchment liming
• ISSN: 0378-1127; 1872-7042; 1872-7042
• DOI: 10.1016/j.foreco.2009.04.030

Whole catchment liming or forest liming has been proposed and implemented as a countermeasure to the effects of elevated sulphur deposition. Since the end of the 1980s the Swedish Forest Agency has undertaken experimental forest liming experiments in selected catchments in southern Sweden. These studies were with low doses (3tonnesha−1) of lime (CaCO3) and dolomite (CaMg(CO3)2). Data from both soil samples and stream water samples have been collected for the 16 years following treatment. The stream data has been complemented with data from untreated catchments, from the Swedish monitoring stream network. Significant differences due to treatment were seen for Ca, cation exchange capacity (CEC) and base saturation (BS) in the humus layer, none of these variables showed a statistically significant change in the mineral soil due to treatment alone. Soil samples from both the treated and untreated sites showed temporal changes in both the humus layer and the mineral soils with increases in pH, Ca and CEC and decreases in BS and Al which were independent of treatment. A combination of treatment and time, gave significant changes in BS and TA down to 10cm in the mineral soil. In the stream water samples no statistically significant differences were observed between treated and untreated sites. Regardless of treatment, the streams exhibited a general pattern of declining concentrations of SO4, Ca, sum of base cations (BC) and increasing acid neutralizing capacity (ANC). In summary, the application of a low dose of lime (3tonnesha−1) did not result in significant changes in surface water chemistry in the study catchments and changes in soil chemistry were mainly restricted to the humus layer during the 16 years following treatment. The natural recovery, as a result of reductions in sulphur deposition, dominated the effects and was clearly seen in both the treated and untreated study sites. MAGIC simulations indicate that this recovery will continue in the coming decades.