Terraced landscapes in Slovakia

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

Factors affecting the persistence of traditional agricultural landscapes in Slovakia during the collectivization of agriculture

Collectivization of agriculture (1950s-1970s) was one of the most important periods in landscape development in Slovakia. Traditionally managed agricultural landscapes, that covered more than half of the Slovak territory, were transformed into large-scale fields and only fragments of traditional agricultural landscapes survived. We mapped the remaining traditional agricultural landscapes using aerial photos and historical maps. We then statistically analyzed the various geographical factors and their influence on the transformation process of traditional and collectivized fields, i.e., slope steepness, soil fertility, distance from settlements and isolation from regional capital cities. The comparison was performed using classification tree analysis. We constructed a set of decision rules that explain why fields were managed traditionally or collectivized. Our findings show that traditional agricultural fields were more likely to persist on steep terrain, less fertile soils, and on locations that were closer to the settlements, but more isolated from the regional capital cities. Steepness played the most important role: small-scale fields located on steep areas were not accessible to heavy machinery and therefore, frequently survived the collectivization. We show that the selected geographical factors are good explanatory variables for the collectivization of arable fields and orchards. For vineyards and grasslands, however, the explanatory power of the selected geographical factors is lower, and we suspect that other factors, not depicted in the analysis play an important role

Assessment of landslide risk using gis and statistical methods in kysuce region

The landslide susceptibility was assessed based on multivariation analysis. The input parameters were represented by lithology, land use, slope inclination and average annual precipitation. These parameters were evaluated as independent variables, and the existing landslides as dependent variables. The individual input parameters were reclassified and spatially adjusted. Spatial analysis resulted in 15 988 combinations of input parameters representing the homogeneous condition unit (HCU ). Based on the landslide density within individual units, the HCU polygons have been classified according to landslide risk into stable, conditionally stable, conditionally stable and unstable (subdivided into low, medium and high landslide risk). A total of 2002 HCU s were affected by landslides, and the remaining 13 986 were not affected. The total HCU area affected by landslides is about 156.92 km2 (20.1%). Stable areas covered 623.01 km2 (79.8%), and conditionally stable areas covered 228.77 km2 (29.33% out of this area). Unstable areas were divided into three levels of landslide risk - low, medium and high risk. An area of 111.19 km2 (14.3%) represents low landslide risk, medium risk 29.7 km2 (3.8%) and 16.01 km2 (2%) represents high risk. Since Zlín Formation lithological unit covers approximately one-third of the study area, it also influences the overall landslide risk assessment. This lithological formation covers the largest area within all landslide risk classes as well as in conditionally stable areas. The most frequent slope class was in the range of 14-19. The higher susceptibility of Zlín Formation to landslides is caused mainly by different geomorphological value of claystone and sandstone sequence. The higher share of claystone results in higher susceptibility of this formation to exogenous degradation processes

Territorial Systems of Ecological Stability in Land Consolidation Projects (Example of Proposal for the LSES of Klasov Village, Slovak Republic)

The observation of spatial and functional relations within ecosystems (Forman, Godron, 1993; Michal, 1994; Jongman, 1995 a,b) and Territorial Systems of Ecological Stability and their design have a successful history not only in the Czech Republic, Germany, Austria, Hungary but also in Slovakia and other countries. The main principle of their design is to create an ecological network in intensively utilised landscape through revitalisation of the existing natural habitats and creation of new ones along with the proposal of their protection and management. The presented contribution represents an example of the proposed spatial framework of ecological stability and management measures in the cadastral area of Klasov. The cadastral area is characterised by prevailing large-block arable parcels and viticultural history. In spite of the agricultural character of the landscape, there are also areas with dispersed non-forest woody vegetation, preserved bank vegetation along streams, wetlands with reed associations, forest growths and mosaics of old abandoned orchards and vineyards as the potential elements of the proposed spatial framework of ecological stability. A functional LTSES framework and implementation of the system of ecostabilizing measures may contribute to increasing diversity of the territory and improvement of its spatial ecological stability. Efforts aimed at the recovery of vine-growing tradition represent a positive feature in terms of increased diversity in the territory

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

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

Rozvoj strategie ochrany tradičních zemědělských krajin založené na komplexním krajinně-ekologickém hodnocení (na příkladu horské krajiny na Slovensku)

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DEVELOPING A STRATEGY FOR THE PROTECTION OF TRADITIONAL AGRICULTURAL LANDSCAPES BASED ON A COMPLEX LANDSCAPE-ECOLOGICAL EVALUATION (THE CASE OF A MOUNTAIN LANDSCAPE IN SLOVAKIA)

Abstract Traditional agricultural landscapes (TALs