. . "clay particles; wind erosion; soil moisture; wind speed; nonerodible fraction"@en . "Determination of wind erosion intensity on heavy clay soils"@en . "2" . . . . "H\u00FAsek, Petr" . . "CZ - \u010Cesk\u00E1 republika" . . "289705" . "RIV/62156489:43210/10:00157006" . . . "Stanoven\u00ED intenzity v\u011Btrn\u00E9 eroze na t\u011B\u017Ek\u00FDch p\u016Fd\u00E1ch"@cs . "Acta Universitatis agriculturae et silviculturae Mendelianae Brunensis : Acta of Mendel University of agriculture and forestry Brno = Acta Mendelovy zem\u011Bd\u011Blsk\u00E9 a lesnick\u00E9 univerzity v Brn\u011B" . . . "Jare\u0161, Vladan" . . "Wind erosion occurs practically only on soils with low content of clay particles -- on light-textured soils. Worldwide sporadic occurrence of wind erosion exists also on heavy clay soils, which could be found in the area of South-eastern Moravia in the foothills of the B\u00EDl\u00E9 Karpaty Mountain, Czech Republic. The research took place here during 2008--2009, which had to determine the intensity of wind erosion. An experimental locality Kr\u00E1sn\u00E9 pole in the cadastral area Ostro\u017Esk\u00E1 Nov\u00E1 Ves was chosen. The intensity of wind erosion was found out in three ways -- from the Map of potential vulnerability of agricultural soils to wind erosion according to cadastral areas, from the calculation of potential erodibility of soil by wind, and from field measurements and subsequent calculation of real erodibility of soil by wind. It was found out during field reconnaissance that wind erosion in the experimental area really exists, although according to the Map of potential vulnerability of soil by wind, the area belon"@en . "3"^^ . . . "P(QH82099)" . "[F0FF543FB2FD]" . . . "1211-8516" . . "3"^^ . "V\u011Btrn\u00E1 eroze se t\u00E9m\u011B\u0159 v\u00FDhradn\u011B vyskytuje na p\u016Fd\u00E1ch s n\u00EDzk\u00FDm obsahem j\u00EDlnat\u00FDch \u010D\u00E1stic -- na p\u016Fd\u00E1ch lehk\u00FDch. Ve sv\u011Btov\u00E9m m\u011B\u0159\u00EDtku je v\u0161ak ojedin\u011Bl\u00FD v\u00FDskyt v\u011Btrn\u00E9 eroze i na p\u016Fd\u00E1ch t\u011B\u017Ek\u00FDch, ke kter\u00E9mu doch\u00E1z\u00ED na jihov\u00FDchodn\u00ED Morav\u011B v podh\u016F\u0159\u00ED B\u00EDl\u00FDch Karpat. V letech 2008--2009 zde prob\u011Bhl v\u00FDzkum, kter\u00FD m\u011Bl za \u00FAkol zjistit intenzitu v\u011Btrn\u00E9 eroze. Jako experiment\u00E1ln\u00ED lokalita byla vybr\u00E1na poln\u00ED tra\u0165 Kr\u00E1sn\u00E9 pole v katastr\u00E1ln\u00EDm \u00FAzem\u00ED Ostro\u017Esk\u00E1 Nov\u00E1 Ves. Intenzita v\u011Btrn\u00E9 eroze zde byla zji\u0161\u0165ov\u00E1na t\u0159emi zp\u016Fsoby -- jednak na z\u00E1klad\u011B Mapy potenci\u00E1ln\u00ED ohro\u017Eenosti zem\u011Bd\u011Blsk\u00FDch p\u016Fd v\u011Btrnou eroz\u00ED podle katastr\u016F, jednak v\u00FDpo\u010Dtem potenci\u00E1ln\u00ED ztr\u00E1ty p\u016Fdy v\u011Btrnou eroz\u00ED a d\u00E1le ter\u00E9nn\u00EDm m\u011B\u0159en\u00EDm a n\u00E1sledn\u00FDm v\u00FDpo\u010Dtem eroze skute\u010Dn\u00E9. P\u0159i ter\u00E9nn\u00EDm pr\u016Fzkumu bylo zji\u0161t\u011Bno, \u017Ee v\u011Btrn\u00E1 eroze se ve zkouman\u00E9 lokalit\u011B vyskytuje, a\u010Dkoli podle Mapy potenci\u00E1ln\u00ED ohro\u017Eenosti p\u016Fd v\u011Btrnou eroz\u00ED spad\u00E1 lokalita do kategorie p\u016Fdy neohro\u017Een\u00E9 a soused\u00ED s kategori\u00ED p\u016Fdy n\u00E1chyln\u00E9. Potenci\u00E1ln\u00ED erodovatelnost p\u016Fdy v\u011Btrem je z\u00E1visl\u00E1 na obsahu j\u00EDlnat\u00FDch"@cs . . "Stanoven\u00ED intenzity v\u011Btrn\u00E9 eroze na t\u011B\u017Ek\u00FDch p\u016Fd\u00E1ch" . "Stanoven\u00ED intenzity v\u011Btrn\u00E9 eroze na t\u011B\u017Ek\u00FDch p\u016Fd\u00E1ch" . "Kozlovsky Dufkov\u00E1, Jana" . "6"^^ . "43210" . "Stanoven\u00ED intenzity v\u011Btrn\u00E9 eroze na t\u011B\u017Ek\u00FDch p\u016Fd\u00E1ch"@cs . "Determination of wind erosion intensity on heavy clay soils"@en . "LVIII" . "RIV/62156489:43210/10:00157006!RIV11-MZE-43210___" . "V\u011Btrn\u00E1 eroze se t\u00E9m\u011B\u0159 v\u00FDhradn\u011B vyskytuje na p\u016Fd\u00E1ch s n\u00EDzk\u00FDm obsahem j\u00EDlnat\u00FDch \u010D\u00E1stic -- na p\u016Fd\u00E1ch lehk\u00FDch. Ve sv\u011Btov\u00E9m m\u011B\u0159\u00EDtku je v\u0161ak ojedin\u011Bl\u00FD v\u00FDskyt v\u011Btrn\u00E9 eroze i na p\u016Fd\u00E1ch t\u011B\u017Ek\u00FDch, ke kter\u00E9mu doch\u00E1z\u00ED na jihov\u00FDchodn\u00ED Morav\u011B v podh\u016F\u0159\u00ED B\u00EDl\u00FDch Karpat. V letech 2008--2009 zde prob\u011Bhl v\u00FDzkum, kter\u00FD m\u011Bl za \u00FAkol zjistit intenzitu v\u011Btrn\u00E9 eroze. Jako experiment\u00E1ln\u00ED lokalita byla vybr\u00E1na poln\u00ED tra\u0165 Kr\u00E1sn\u00E9 pole v katastr\u00E1ln\u00EDm \u00FAzem\u00ED Ostro\u017Esk\u00E1 Nov\u00E1 Ves. Intenzita v\u011Btrn\u00E9 eroze zde byla zji\u0161\u0165ov\u00E1na t\u0159emi zp\u016Fsoby -- jednak na z\u00E1klad\u011B Mapy potenci\u00E1ln\u00ED ohro\u017Eenosti zem\u011Bd\u011Blsk\u00FDch p\u016Fd v\u011Btrnou eroz\u00ED podle katastr\u016F, jednak v\u00FDpo\u010Dtem potenci\u00E1ln\u00ED ztr\u00E1ty p\u016Fdy v\u011Btrnou eroz\u00ED a d\u00E1le ter\u00E9nn\u00EDm m\u011B\u0159en\u00EDm a n\u00E1sledn\u00FDm v\u00FDpo\u010Dtem eroze skute\u010Dn\u00E9. P\u0159i ter\u00E9nn\u00EDm pr\u016Fzkumu bylo zji\u0161t\u011Bno, \u017Ee v\u011Btrn\u00E1 eroze se ve zkouman\u00E9 lokalit\u011B vyskytuje, a\u010Dkoli podle Mapy potenci\u00E1ln\u00ED ohro\u017Eenosti p\u016Fd v\u011Btrnou eroz\u00ED spad\u00E1 lokalita do kategorie p\u016Fdy neohro\u017Een\u00E9 a soused\u00ED s kategori\u00ED p\u016Fdy n\u00E1chyln\u00E9. Potenci\u00E1ln\u00ED erodovatelnost p\u016Fdy v\u011Btrem je z\u00E1visl\u00E1 na obsahu j\u00EDlnat\u00FDch" . .