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of Aporrectodea caliginosa, emerge new earthworm species noncharacteristic to the<br />
pine forest soils. Here are formed 3 to 4 earthworm species communities, who are<br />
characteristic both- to conifer, and deciduous tree forests. They are considered as a<br />
transition type species communities characterizing forest eutrophication processes. In<br />
the non-eutrophicated pine forest soils such species communities have not been<br />
found.<br />
3.5. Earthworm communities change due to the industrial pollution in the pine<br />
forests near Saulkalne<br />
Saulkalne dolomite processing plant yearly emits into the atmosphere more<br />
than 700 t of pollutants. In the 80’s of the last century, the production units<br />
functioned in full load, but in the turn of the 80’s and 90’s, the production capacity<br />
was rapidly decreased. The most common pollutants in the exausted emissions of the<br />
factory are the dust containing calcium and magnesium compounds. Till 1995, when<br />
installation of inovative purification filters was initiated the company operated<br />
without strict requirements on the environmental protection (Vaivara, 2006).<br />
3.5.1. Description of the sampling plots and sampling procedure<br />
In order to determine the effect of the pollution created by Saulkalne dolomite<br />
processing plant, in 1989 near the industrial area of Saulkalne were initiated lasting<br />
observations on the forest dynamic. In the dominant wind direction for 6.3 km was<br />
established transect with 5 sampling plots at different distances from the dolomite<br />
processing factory (Table 3.4).<br />
The sampling plots were created in areas, which conform to Vaccinio myrtilli –<br />
Pinetum forest growth type. The forest stand age in 1989 was assessed to be from 41<br />
to 63 years. Earthworms were sampled in the period from 1989 to 1991. The soil of<br />
the sampling plots is formed of fine-grained sand. Organic matter and humus<br />
accumulation horizon number in the first two sampling plots, closest to the emission<br />
source, is higher (O, Ah, AhE). In these sampling plots, mineralization of the organic<br />
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