REGULARITIES OF ECOLOGOCAL DIFFERENTIATION OF THE SOILS COVER IN THE EAST-SLOVAKIAN LOWLANDS

Authors

  • А. А. Лісняк Kharkiv V.N. Karazin National University, Ukraine
  • Дж. Вілчек Faculty of management University of Presov in Presov, Slovakia
  • Е. Міхаелі Soil Science and Conservation Research Institute Bratislava, regional work place Presov, Slovakia

Keywords:

pedosphere, regularities of ecological differentiation, landscape, soils

Abstract

The character of the soil cover in the landscape is depends on the physical geographic regularities of the differentiation the pedosphere (e.g. horizontal zonation, vertical zonation, detailed ecological differentiation, etc.).With themare associated soil-forming processesto formsoil coverof the regions.East- Slovak Lowlandhas been and isa typicalagrarianecosystem.The intensityof agriculturein that regionis dependent on theproductionofarangeof soil and from inputs toproduction.In our paperwe'll take the quality of the soils, typologically-production categories of the soil - soil-fertility of East-SlovakLowland and also the representation of the soils from aspects ofthe economicprofitability ofcropsandcomparisonthese parameters with the Slovak Republic. In linewith recentMorphogenetic andsoilclassification systemof the Slovak Republicon the territory ofthe East- Slovak Lowland, we can define9soilgroups, 17 typesandseveralsubtypes, varietiesandforms ofsoil. Most of thesoilson theEast-Slovak Lowlandsare usesas agricultural land, till 69 % of the territory, of which 68 %isarable land. It is grownhere especiallydensely sowingcereal crop(37 %), followed by grain maize(10 %), legumes (5 %), oil plants (10 %), sugar beet (5 %), annual fodder (8 %), perennial fodder products (8 %).

The soil cover on the East-Slovakian plain is different from the soil cover of East- Slovakian hilly country. While for the soil cover differentiation of East-Slovakian plain is applies mainly azonation (substrate-morphological-hydrological conditions) for the differentiation the soil cover of East-Slovakian hilly country is applies above all of barrier zonation and only partially azonation (Podvihorlatská hilly country). Theregularitiesandconditions are significantlyaffecting the fertility of agricultural soils and land use of the landscape. From the aspect offertilityaredominated here productive category of soilsO3(veryproductive soils).

References

Baňacký, V. et al. 1989. Geological maps of the north and south part of the East-Slovakian Lowland and the Zemplínske hill (1: 50 000). GUDŠ, Bratislava (in Slovak and English).

Džatko, M. et al. 2002. Evaluation of the produc-tive potential of agricultural soils and soil ecologi-cal regions of Slovakia. VÚPOP, Bratislava, p. p. 87 (in Slovak).

Mazúr, E., Lukniš, M., 1980: Geomorphological units 1:500 000 (in Slovak), map No 16. Atlas SSR, SAVa SÚGK, Bratislava, p. 54-55.

Lapin, M., Faško, P., Melo, M., Šťasnź, P., Tomlain, J. 2002. Klimatické oblasti, map No 27. In: Atlas krajiny SR. Bratislava: MŽP SR, 2002. s. 95. ISBN 80-88833-27-2.

Šály et al., 2000. Morphogenetic-classification system of the soils of the Slovak Republic. VÚPOP, Bratislava, p.p. 74 (in Slovak).

Vilček, J. 2011. Potential and quality parameters of agricultural soils of Slovakia. Geographical jour-nal, 63: 2, p. 133 -154 (in Slovak).

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Published

2015-01-28