Abstract
In conclusion, the following major findings can be stated:
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High deposition loads of air pollutants in the past caused high accumulation rates of the respective substances in the soil; locally base saturation and pH values of the soils were improved, also Ca, S, and N soil stores were increased; as a consequence, humus forms changed.
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In relation to former deposition loads, high output rates still occur from the rooted solum, particularly related to SO42‒, Ca2+, and at Taura — because of subsoil acidification — also Al3+.
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Despite regionally high historic N deposition rates and N input via fertilization no N-losses with the seepage water could be detected.
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The strong reduction of the alkaline deposition loads after reunification of Germany and the still relatively high acid deposition rates locally lead to re-acidification of soils.
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Reduced concentrations of air pollutants in the atmosphere after reunification of Germany led to an improvement of canopy density and foliar tissue of the investigated Scots pine stands.
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The improvement of the photosynthetic potential of the foliage is related to an enhanced growth performance of the trees.</Absttext>
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© 1998 Springer Science+Business Media Dordrecht
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Bellmann, K., Hüttl, R.F. (1998). Concluding remarks. In: Hüttl, R.F., Bellmann, K. (eds) Changes of Atmospheric Chemistry and Effects on Forest Ecosystems. Nutrients in Ecosystems, vol 3. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-9022-8_17
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DOI: https://doi.org/10.1007/978-94-015-9022-8_17
Publisher Name: Springer, Dordrecht
Print ISBN: 978-90-481-5224-7
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