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primary production and nitrogen uptake (Huhta et al., 1998). In the areas where lime<br />

has been applied, nitrogen mineralization happens even 50 times faster than in the<br />

areas where lime has not been applied. These processes are more active after<br />

introduction of the earthworm species Aporrectodea caliginosa (Robinson et al.,<br />

1992b). Earthworms have positive impact on microorganisms of the forest soils.<br />

They favor mycorriza formation and facilitate plant growth (Haimi, Einbork, 1992).<br />

By increase of earthworm density and introduction of new species due to lime<br />

application, increases also earthworm impact on the soil processes. Earthworms are<br />

an essential factor in humus formation processes. Consequently changes the podsol,<br />

and mull humus begins to form (Lee, 1985; Deleporte, Tillier, 1999). Dendrobaena<br />

octaedra brakes down borders between the organic layers of the soil, mixing the<br />

upper horizons of organic matter. Aporrectodea sp., Lumbricus rubellus, L.terrestris<br />

intensively mixes the upper ground cover layers with mineral layers in depth of 25 to<br />

30 cm, what to a certain extent may be compared to a tillage. In the boreal forest<br />

areas of the USA, introducing in the forest soils different earthworm species at the<br />

same time, in the organic horizon of the soil was observed soil raw humus (mor)<br />

transformation into a mull structure with a well formed Ah horizon rich in organic<br />

matter (Frelich et al., 2006).<br />

3.3. Latvia’s boreal pine forest eutrophication and transformation<br />

During the last decades intensive changes have been observed in Latvia’s pine<br />

forest vegetation due to atmospheric deposition, climate changes, and land utilization<br />

changes. Pine forest plant societies become less stable, numerous uncharacteristic<br />

foreign species aggressively spread among them. Due to intensive spread of<br />

gramineae species in the forests, enhances formation of sod. Organic matters<br />

agglomerate in the upper layer of the soil, thus obstructing regeneration of conifer<br />

trees (Laiviņš, Laiviņa, 1991; Laiviņš, 1998). Great impact is also of transboundary<br />

transfer of the pollution (including nitrogene compounds) and emission from the<br />

local pollution sources. Intensive use of dolomite and limestone in construction and<br />

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