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Trends in soil water composition at a heavily polluted site - effects of decreased S-deposition and variations in precipitation

Academic lecture
Year of publication
2000
External websites
Cristin
Involved from NIVA
Rolf David Vogt
Contributors
Rolf David Vogt, Hans Martin Seip, Hege Orefellen, Gunnar Skotte, Christina Irgens, Jan Tyszka

Summary

Precipitation, soils and soil water in a forested catchment in western Poland have been studied during the period 1992 - 96 (see also Vogt et al., this conf.). The S-deposition in the area during the study period was 2 - 3g S m-2 yr-1. In spite of decreasing anthropogenic emissions the S-deposition in the area did not change much during the study period mainly because the first years were exceptionally dry. However, the S-deposition was considerably higher during the previous decade. Based on soil water sulphate concentration, pH, acid neutralising capacity and the ratio of Al3+/(Ca2+ + Mg2+), there is apparently an amelioration in the conditions. A study using inter alia principal component analysis, indicates that this improvement is mainly due to more precipitation in the later part of the study period. Variations in precipitation amount have a pronounced effect on the soil-water chemistry, which makes it difficult to establish trends caused by changes in anthropogenic deposition. Long time series are therefore necessary to establish recovery due to reduced S-emissions.