Published in Scientific Papers. Series A. Agronomy, Vol. LXII, Issue 2
Written by Violeta VALCHEVA, Nedialka YORDANOVA, Krasimir TRENDAFILOV
The study was carried out on terrains located in Ginot and Vodenichane villages, on a total area of 152.2 hectares. As a result of the study in the investigated terrains, were established the following soil differences - Pelic vertisols, Peligleyic vertisols, Chromi-eutric cambisols, Eutric regosols, Rankers. The lands of Ginot village occupies a total area of 39 hectares in the high western part and 10 hectares in the lower eastern part, which borders the river Tarnavska. In the western part the terrain was well drained, including the areas of the relatively shallow gully in a direction from the northeast to the southwest. The following massifs were studied on the land of the village of Vodenichane: M 160 occupied a high and generally drained terrain, where the deep and well developed soils occupy about 24% and the rest occupied with shallow and stony soils; М 100 is a complex landscape which can be divided into drained and not drained parts. The slightly drained and not drained part of the terrain occupied an area of 9 hectares in the eastern part of the site; M 210 - the whole area was a low not drained or slightly drained area. The groundwater level was high.
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