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This article in JEQ

  1. Vol. 25 No. 1, p. 110-119
    Received: Oct 18, 1994

    * Corresponding author(s): reiner.giesler@sek.slu.se
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Reversing Acidification in a Forested Catchment in Southwestern Sweden: Effects on Soil Solution Chemistry

  1. Reiner Giesler *,
  2. Filip Moldan,
  3. Ulla Lundström and
  4. Hans Hultberg
  1. IVL, Swedish Environmental Research Inst., Dep. of Ecology and Environmental Research, Box 47086, S-40258 Gothenburg, Sweden.



The exclusion of acid precipitation in whole-catchment experiments can provide valuable information to further our understanding of recovery processes of acidified soils. In this study, we focused on the reversibility of acidification-induced changes in different soil horizons when anthropogenic deposition was excluded. A small forested catchment in the Gårdsjön area in southwest Sweden was covered with a transparent roof in April 1991 and sprinkled with water that simulated preindustrial deposition levels. Within the roofed catchment and a reference catchment the soil solution was studied using a centrifugation drainage technique. Sulfate concentrations in the O and E horizons decreased by 75 and 65%, respectively, within 3 mo after treatment. In the Bs horizon, the sulfate concentration decreased more gradually, reaching about 52% of the pretreatment level in 1993 after 2.5 yr of treatment. The decline in sulfate concentrations in the runoff followed the pattern observed in the Bs horizon. The net loss from the catchment during the first 2.5 yr of the treatment period represents approximately 9% of the phosphate-extractable sulfate pool. No increase in soil solution pH occurred until 1994. In 1993, Al concentrations were lower compared with those found in earlier samplings of the soil solution and runoff. Fluctuations in Al concentrations were correlated most strongly with changes in ionic strength in the soil solution and runoff. Nitrate concentrations remained unchanged in the soil solution and runoff. Concentrations of NO3 were, however, already low (<30 µmol L−1) before the exclusion.

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