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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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