6 research outputs found

    Terraced landscapes in Slovakia

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    This study investigates the distribution of terraced landscapes in Slovakia and analyzes their structural characteristics and land use. We found that traditional farming and terrace building as a part of agricultural intensification resulted in two types of terraced landscapes: historical terraced landscapes and new terraced landscapes. The two types differ in size, structure of various elements, their management intensity, and the impact of these spatial structures on biodiversity. Historical terraced landscapes in Slovakia have been partially preserved in vineyard regions, but they are mainly found in mountainous areas. New terraced landscapes are mainly linked to vineyard landscapes. The plant species composition on the mapped terraced landscapes shows a high diversity of habitats and terraces as agrarian relief forms create islands of species diversity in extensively managed agricultural landscapes

    Small Woodlands and Trees in Traditional Agricultural Landscapes of Slovakia

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    The studies focused on distribution and characteristic of small woodlands and trees as a typical feature of traditional agricultural landscapes (TAL) in Slovakia are missing or are rather local. The source data for this study was obtained from the national inventory of TAL performed in 2010-2012 in Slovakia, where woody vegetation was considered as one of the landscape elements creating mosaic of TAL. Based on the types of woodland present, which endow the landscape with a distinctive character and structure, we have divided TAL into five subtypes: 1) TAL with low occurrence of woodland – not more than 10 % of the site covered by woods, 2) TAL with spatial woodland formation, 3) TAL with solitaire trees dominant, 4) TAL with lines of trees or shrubs dominant, and 5) TAL with small woodland dominant

    Impact of Historical Agrarian Landforms on Soil Water Content Variability at Local Scale in West Carpathian Region, Slovakia

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    The historical agrarian landforms (AL) represent man-made features that alter the hydrological process on cultivated hillslopes. Soil water content (SWC) and its spatial and temporal variability represent an important state indicator for understanding of these processes. In order to assess the differences between individual AL in terms of SWC stability, continuous soil moisture measurements at five different monitoring localities characterized by a specific combination of AL and environmental factors were performed. Temporal SWC stability was evaluated using mean relative difference (MRD) and its standard deviation (SDRD). Differences in mean SWC and MRD values demonstrated the difference between saturated inner part of the AL and external parts such as terraced slopes and mounds, soil depths, and slope positions. In order to analyze the relationship between SWC and environmental variables, the methods of constrained ordination were applied. The most influential factors that regulate SWC variability during the periods of rain were identified as: stone content, sand fraction content, slope orientation, type of agrarian landform, and its orientation against the contour lines. Results also pointed to the fact that different factors predominate among individual localities and, therefore, SWC variability reflects the effect of combination of various environmental factors rather than effect of single parameter. Besides the improved understanding of SWC variability, our results also highlight the importance of AL in regulating the hydrological processes at historical agricultural landscape of the West Carpathian region
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