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Environmental aspects of relief transformation (Silesian Upland, Southern Poland)

100%

Pełka-Gościniak J.

nr 4

13-20

The geological structure and the occurrence of mineral resources in the Silesian Upland in a significant way influenced the development of industry and caused transformation of every landscape element, among others changes in relief and therefore the formation of anthropogenic landforms. The paper focuses on environmental aspects of relief transformation in the Silesian Upland. The author described aesthetic, geomorphological, hydrological, climatological, pedological and biological aspects on the base of representatives of two groups of landforms–consciously created by human being and being an unintentional effect of human activity (of secondary character). All analysed landforms are new elements in relief, in majority of cases being in disharmony with their neighbourhood. They are alien to the landscape and disturb the equilibrium in the nature. It was proved that they strongly influence water and climatological conditions and soil cover. But sometimes the anthropogenic landforms can be perceived as advantageous for the nature, especially in case of subsidence depressions because of development of aquatic and hydrophilous species and in case of spoil tips due to spontaneous development of vegetation cover. The nature easily adapts to new environmental conditions (process of natural succession and independent introduction of species for new habitats). In these terrains the increase in biodiversity was observed.

Zastosowanie metody inwersji danych z pomiarów elektrooporowych do oceny stanu termicznego hałdy pogórniczej w Chorzowie

58%

Kotyrba A. , Siwek A.

tom Vol. 65, nr 8

496--504

Air conditions in post-mining areas are threatened by thermal activity of old spoil tips of coal mines. Reclamation operations cause only time-limited suppression of the oxidation process of carbon particles in the spoil heap. There are different reasons for that process. One of them is the incorrectly recognized geometry of the combustion spots in the spoil tip mass and the ways in which they are powered by oxygen from the atmosphere. The 1D inversion of vertical resistivity sounding data (VES) allows visualizing the down-going thermal effects and concluding about transport of atmospheric air (oxygen) and combustion gases in the whole mass. The resistivity distribution within waste can effectively support interpretation of geochemical and geothermic observations made on the spoil tip. The article describes the results of resistivity measurements made on an old spoil tip with waste from coal production in a heavy urbanized area of Chorzów City. Currently, the area of the former spoil heap is used for recreation and sports purposes (a park).