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Czasopismo

2001 | 50 |

Tytuł artykułu

Mutual relations between soil cover and plants in mountainous humid climatic conditions

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Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
Specific, humid climate of mountain areas has a great influence on the properties of soils and vegetation, as well as on the mutual relations between these inseparable elements of ecosystems. Research on the interdependence between soils and natural vegetation was carried out on ' the mountain meadows of the Bieszczady National Park. In conditions of the cooler and more humid mountain climate the peculiar character of the soils lies in the presence of organic surface horizon of properties varying considerably from the properties of deeper mineral horizons. This horizon is of great importance in the protection of scarce elements. It prevents pollutants from reaching the ecosystem. It influences the soil water economy. It prevents erosion. This buffer element of the mountain soils requires special protection - in the Bieszczady Mountains the erosion of the mountain meadow soils is only noticeable where the covering vegetation and the organic surface soil horizon were destroyed, e.g. on tourist tracks. The plants of the Bieszczady mountain meadows, together with their direct product - the organic surface soil horizon, prevents the chemical erosion of the mountain meadows, reducing the leaching of many biogenous elements, e.g. calcium.

Wydawca

-

Czasopismo

Rocznik

Tom

50

Opis fizyczny

p.253-261

Twórcy

autor
  • Agricultural University of Krakow, Cwiklinskiej 2, 35-601 Rzeszow, Poland

Bibliografia

  • 1. Adamczyk B.: Studies on the development of relations between parent rock and soils. Part II. Forest soils formed on Flysch rocks of the Magura nappe in the Gorce Mts. Acta Agraria et Silvestria, Ser. Silv., VI, 3-46, 1966.
  • 2. Kostur R., Kopeć S.: Importance of permanent grasslands in the water economy of mountains. Zesz. Probl. Post Nauk Roln., 235, 165-175, 1980.
  • 3. Malicki M,: Some notes on physiography of the Flysch Carpathians. Roczn. Glebozn., 13, 3-25, 1963.
  • 4. Skiba S., Drewnik M., Szmuc R., Prędki R.: The buffering properties of the mountain grassland soils in the Western Bieszczady Mis, Roczn. Bieszczadzkie, 2, 193-199, 1993.
  • 5. Skiba S., Drewnik M., Prędki R., Szmuc R,: Soils of the Bieszczady National Park. Monografie Bieszczadzkie, 2, 1-88, 1998.
  • 6. Skiba S., Winnicki I.: Soil of the plant communities of the mountain meadows in the Bieszczady Mts. Roczn. Bieszczadzkie, 4, 97-109, 1995.
  • 7. Starkel Ł.: Soil erosion versus water economy in the Carpathians. Zesz. Probl. Post. Nauk Roln., 235, 103-118, 1980.
  • 8.Uziak S.:The origin and classification of mountain soils in the Flysch Carpathian. Roczn. Glebozn., 13, 56-71, 1963a.
  • 9. Uziak S.: Brown soils of mountain regions, exemplified by soils of the Western Bieszczady. Ann. UMCS, E, 13, 37-54, 1963 b.
  • 10. Woźniak L.: Organogenic metal elements and some toxic heavy metals in soils and plants of Bieszczady. Zesz. Nauk AR Kraków, Rozprawy, 216, 1-80, 1996.
  • 11.Woźniak L.: Selected problems of elements cycling in Bieszczady mountain meadows environment. Zesz. Probl. Post. Nauk Roln., 464, 179-190, 1998.

Typ dokumentu

Bibliografia

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bwmeta1.element.agro-article-6ebea2bc-1ce9-4274-9f41-607068a769c2
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