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Volume XL (40)

 

 

Tadeusz Ciupa 

Hydrological effects of urbanization as exemplified by the Silnica and Sufraganiec river catchments (Kielce, Poland)

Ciupa T., 2009, Hydrological effects of urbanization as exemplified by the Silnica and Sufraganiec river catchments (Kielce, Poland), Folia Geographica ser. Geographica-Physica, vol. XL (40): 5-25.

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Matthias Kändler, Christina Seidler 

Hydrochemical load in a small river following heavy rain events

Kändler M., Seidler C., 2009, Hydrochemical load in a small river following heavy rain events, Folia Geographica ser. Geographica-Physica, vol. XL (40): 27-32.

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Ladislav Holko, Helena Hlavatá, Zdeněk Kostka, Ján Novák 

Hydrological regimes of small catchments in the High Tatra mountains before and after extraordinary wind-induced deforestation

Holko L., Hlavatá H., Kostka Z., Novák J., 2009, Hydrological regimes of small catchments in the High Tatra mountains before and after extraordinary wind-induced deforestation, Folia Geographica ser. Geographica-Physica, vol. XL (40): 33-44.

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Anna Maria De Girolamo, Antonio Lo Porto, Gerardina Santese 

Development of an alternative scenario in a small mediterranean basin using the rainfall-runoff swat model

De Girolamo A.M., Lo Porto A., Santese G., 2009, Development of an alternative scenario in a small mediterranean basin using the rainfall-runoff swat model, Folia Geographica ser. Geographica-Physica, vol. XL (40): 45-56.

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Pavla Pekarova, Milan Onderka, Pavol Miklanek, Dana Halmova, Jan Pekar 

Mass balance of dissolved chemicals in microbasins with different land cover

Pekarova P., Onderka M., Miklanek P., Halmova D., Pekar J., 2009, Mass balance of dissolved chemicals in microbasins with different land cover, Folia Geographica ser. Geographica-Physica, vol. XL (40): 57-70.

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Dominika Krzemińska (Prądzyńska), Thom Bogaard, Martijn Westhoff 

Spatial and temporal variability of soil moisture patterns related to preferential flow measured using distributed temperature sensing

(Prądzyńska) D.K., Bogaard T., Westhoff M., 2009, Spatial and temporal variability of soil moisture patterns related to preferential flow measured using distributed temperature sensing, Folia Geographica ser. Geographica-Physica, vol. XL (40): 71-78.

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Tomasz Zaleski 

Pedogenetic conditions affecting hydrophysical properties of luvisols derived from loess

Zaleski T., 2009, Pedogenetic conditions affecting hydrophysical properties of luvisols derived from loess, Folia Geographica ser. Geographica-Physica, vol. XL (40): 79-89.

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Marcin Żyła 

Water and air properties of eroded loess soils of the Proszowice Plateau

Żyła M., 2009, Water and air properties of eroded loess soils of the Proszowice Plateau, Folia Geographica ser. Geographica-Physica, vol. XL (40): 91-103.

Keywords: initial loess soils, chernozems, erosion, water and air properties

Summary: Loess-based soils are characterized by high agricultural value and have been cultivated since the Neolithic. Intensive agricultural activity has transformed these soils, especially due to intensified erosion processes. The aim of this paper is to present the basic water and air properties of the investigated soils, namely: soil solid phase density, bulk density, capillary water capacity, total porosity, and air capacity. The research presented herein includes chernozems at different stages of erosion-based transformation compared to strongly eroded initial loess soils from the Proszowice Plateau.
Erosion processes in the research area have brought about a transformation of soil profile morphology and have partially influenced its water and air properties. The most important transformation in initial loess soils is the lack of subsurface transitional horizons which offer the best conditions for plant growth and play a very important role in supplying water and air to plants. The research presented herein shows that during the analysis of the physical properties of surface horizons (Ap, Akp), care needs to be taken to account for the period of sampling due to seasonal agricultural activity that affects soil's physical properties. In the deeper soil horizons, this is not an important issue as agricultural activity is performed at limited depths (ca. 20?35 cm).

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Roman Cieśliński  

Differences in chloride concentration in the outlets of rivers and canals in the southern Baltic coastal region during normal and extreme weather conditions

Cieśliński R., 2009, Differences in chloride concentration in the outlets of rivers and canals in the southern Baltic coastal region during normal and extreme weather conditions, Folia Geographica ser. Geographica-Physica, vol. XL (40): 105-116.

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