With this paper we investigate the effect of sand contribution to organic soils and direct influence of this process on the physical and physicochemical properties on the example of transitional bog in the Stolowe Mountains (the Central Sudetes), which was periodically covered by sand material from sandstone cliffs weathering. Field survey and soil sampling were conducted in August 2015 in the area of Biale Skaly. Soil material for laboratory analysis was collected from three peat cores, while soil samples were collected from each soil horizon distinguished in each core. Obtained results indicate the great impact of mineral material admixture on soil properties, both physicochemical and chemical. Recorded values of each soil parameter in the organic horizons adjacent to the mineral interlayers differ considerably from those obtained in the soil profile free of sand admixtures. Preliminary study of soil cover of transitional bog will allow correct planning of palaeoecological research about genesis and evolution of this peatland.
CITATION STYLE
Glina, B., Waroszewski, J., Bogacz, A., Majewski, W., Kaczmarek, T., Gajewski, P., & Kaczmarek, Z. (2017). Sand removal from sandstone cliffs as the main factor influencing properties of organic soils - A case study of transitional bog in the stołowe mountains. Polish Journal of Soil Science, 50(1), 21–31. https://doi.org/10.17951/pjss.2017.50.1.21
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