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changes dominance structure, Dendrobaena octaedra is replaced by Lumbricus<br />

rubellus. Populations of endogeic Aporrectodea caliginosa form in greatly<br />

eutrophicated biocommunities.<br />

7. Formation of humus horizon in the eutrophicated soils create additional<br />

living-space for earthworms, both with appropriate feeding conditions and possibility<br />

to migrate into deeper layers in case of unfavorable meteorological conditions.<br />

8. Earthwrom activities in the eutrophicated forest soils become an essential<br />

inner factor of the biocenosis, and initiate further soil transformation process.<br />

Earthworms improve physical soil properties, activate breakdown of the organic<br />

matter and their spread into the soil profile, thus promoting formation of thicker<br />

humus horizon. Close to the populated areas establishment of new earthworm<br />

populations occur faster than in isolated forest areas, therefore, in such areas quicken<br />

the forest eutrophication processes.<br />

9. Earthworms are considered as great indicatiors of the oligotrophic pine<br />

forest eutrophication processes. The most important bioindicative indicators in the<br />

initial stages of the eutrophication processes are the total earthworm population<br />

density increase, 3 to 4 species earthworm communities, formation of a stable<br />

Lumbricus rubellus population, and expansion of the ecological group spectrum.<br />

10. Changes in earthworm communities are being detected before visual<br />

changes in the forest phytocenosis. That allows to identify soil eutrophication in its<br />

initial stages.<br />

40

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