Characteristics of some serpentinite soils in Austrian pine stands in the area of Divčibare-Bukovi [Serbia] | Карактеристике неких серпентинских земљишта у састојинама црног бора на подручју Дивчибаре-Букови [Србија]
2008
Кошанин, О., Шумарски факултет, Београд (Serbia) | Гајић, Б., Шумарски факултет, Београд (Serbia)
This paper presents the results of studies of the soil and parent rock, performed in the area of Divčibare-Bukovi: in FMU Maljen-Ridovi, site Lučića Ograde and FMU Bukovi, site Ražana. On serpentinite, depending on the relief, a series of soils is formed such as eutric ranker and eutric brown soil, and illimerised and pseudogleyed soils are formed only exceptionally. In the study area, the following soil units are distinguished: eutric colluvium on serpentinite, eutric humus-siliceous soil on serpentinite and shallow eutric brown soil on serpentinite. The lessivé and pseudogleyed soils are not formed, primarily because of the specific terrain configuration, which is characterised by steep slopes, as well as by relatively high mean annual precipitation (890 mm), which conditions severe erosion processes on the land surface.
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