@article{cebecauerConsequencesLandcoverChanges2008,
  title = {The Consequences of Land-Cover Changes on Soil Erosion Distribution in {{Slovakia}}},
  author = {Cebecauer, Tomáš and Hofierka, Jaroslav},
  date = {2008-06},
  journaltitle = {Geomorphology},
  volume = {98},
  pages = {187--198},
  issn = {0169-555X},
  doi = {10.1016/j.geomorph.2006.12.035},
  url = {https://doi.org/10.1016/j.geomorph.2006.12.035},
  abstract = {Soil erosion is a complex process determined by mutual interaction of numerous factors. The aim of erosion research at regional scales is a general evaluation of the landscape susceptibility to soil erosion by water, taking into account the main factors influencing this process. One of the key factors influencing the susceptibility of a region to soil erosion is land cover. Natural as well as human-induced changes of landscape may result in both the diminishment and acceleration of soil erosion. Recent studies of land-cover changes indicate that during the last decade more than 4.11\,\% of Slovak territory has changed. The objective of this study is to assess the influence of land-cover and crop rotation changes over the 1990-2000 period on the intensity and spatial pattern of soil erosion in Slovakia. The assessment is based on principles defined in the Universal Soil Loss Equation (USLE) modified for application at regional scale and the use of the CORINE land cover (CLC) databases for 1990 and 2000. The C factor for arable land has been refined using statistical data on the mean crop rotation and the acreage of particular agricultural crops in the districts of Slovakia. The L factor has been calculated using sample areas with parcels identified by LANDSAT TM data. The results indicate that the land-cover and crop rotation changes had a significant influence on soil erosion pattern predominately in the hilly and mountainous parts of Slovakia. The pattern of soil erosion changes exhibits high spatial variation with overall slightly decreased soil erosion risks. These changes are associated with ongoing land ownership changes, changing structure of crops, deforestation and afforestation.},
  keywords = {*imported-from-citeulike-INRMM,~INRMM-MiD:c-12687198,agricultural-land,forest-resources,land-cover,slovakia,soil-erosion,soil-resources},
  number = {3-4}
}

{"_id":"4LrR9GmetZuLq5EGd","bibbaseid":"cebecauer-hofierka-theconsequencesoflandcoverchangesonsoilerosiondistributioninslovakia","authorIDs":[],"author_short":["Cebecauer, T.","Hofierka, J."],"bibdata":{"bibtype":"article","type":"article","title":"The Consequences of Land-Cover Changes on Soil Erosion Distribution in Slovakia","author":[{"propositions":[],"lastnames":["Cebecauer"],"firstnames":["Tomáš"],"suffixes":[]},{"propositions":[],"lastnames":["Hofierka"],"firstnames":["Jaroslav"],"suffixes":[]}],"date":"2008-06","journaltitle":"Geomorphology","volume":"98","pages":"187–198","issn":"0169-555X","doi":"10.1016/j.geomorph.2006.12.035","url":"https://doi.org/10.1016/j.geomorph.2006.12.035","abstract":"Soil erosion is a complex process determined by mutual interaction of numerous factors. The aim of erosion research at regional scales is a general evaluation of the landscape susceptibility to soil erosion by water, taking into account the main factors influencing this process. One of the key factors influencing the susceptibility of a region to soil erosion is land cover. Natural as well as human-induced changes of landscape may result in both the diminishment and acceleration of soil erosion. Recent studies of land-cover changes indicate that during the last decade more than 4.11\\,% of Slovak territory has changed. The objective of this study is to assess the influence of land-cover and crop rotation changes over the 1990-2000 period on the intensity and spatial pattern of soil erosion in Slovakia. The assessment is based on principles defined in the Universal Soil Loss Equation (USLE) modified for application at regional scale and the use of the CORINE land cover (CLC) databases for 1990 and 2000. The C factor for arable land has been refined using statistical data on the mean crop rotation and the acreage of particular agricultural crops in the districts of Slovakia. The L factor has been calculated using sample areas with parcels identified by LANDSAT TM data. The results indicate that the land-cover and crop rotation changes had a significant influence on soil erosion pattern predominately in the hilly and mountainous parts of Slovakia. The pattern of soil erosion changes exhibits high spatial variation with overall slightly decreased soil erosion risks. These changes are associated with ongoing land ownership changes, changing structure of crops, deforestation and afforestation.","keywords":"*imported-from-citeulike-INRMM,~INRMM-MiD:c-12687198,agricultural-land,forest-resources,land-cover,slovakia,soil-erosion,soil-resources","number":"3-4","bibtex":"@article{cebecauerConsequencesLandcoverChanges2008,\n title = {The Consequences of Land-Cover Changes on Soil Erosion Distribution in {{Slovakia}}},\n author = {Cebecauer, Tomáš and Hofierka, Jaroslav},\n date = {2008-06},\n journaltitle = {Geomorphology},\n volume = {98},\n pages = {187--198},\n issn = {0169-555X},\n doi = {10.1016/j.geomorph.2006.12.035},\n url = {https://doi.org/10.1016/j.geomorph.2006.12.035},\n abstract = {Soil erosion is a complex process determined by mutual interaction of numerous factors. The aim of erosion research at regional scales is a general evaluation of the landscape susceptibility to soil erosion by water, taking into account the main factors influencing this process. One of the key factors influencing the susceptibility of a region to soil erosion is land cover. Natural as well as human-induced changes of landscape may result in both the diminishment and acceleration of soil erosion. Recent studies of land-cover changes indicate that during the last decade more than 4.11\\,\\% of Slovak territory has changed. The objective of this study is to assess the influence of land-cover and crop rotation changes over the 1990-2000 period on the intensity and spatial pattern of soil erosion in Slovakia. The assessment is based on principles defined in the Universal Soil Loss Equation (USLE) modified for application at regional scale and the use of the CORINE land cover (CLC) databases for 1990 and 2000. The C factor for arable land has been refined using statistical data on the mean crop rotation and the acreage of particular agricultural crops in the districts of Slovakia. The L factor has been calculated using sample areas with parcels identified by LANDSAT TM data. The results indicate that the land-cover and crop rotation changes had a significant influence on soil erosion pattern predominately in the hilly and mountainous parts of Slovakia. The pattern of soil erosion changes exhibits high spatial variation with overall slightly decreased soil erosion risks. 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