"\u010Cl\u00E1nek popisuje Laboratorn\u00ED de\u0161\u0165ov\u00FD simul\u00E1tor Katedry hydromeliorac\u00ED a krajinn\u00E9ho in\u017Een\u00FDrstv\u00ED Fakulty stavebn\u00ED \u010CVUT Praha, princip prob\u00EDhaj\u00EDc\u00EDch experiment\u016F na n\u011Bm (pou\u017E\u00EDvan\u00E9 intenzity simulovan\u00FDch sr\u00E1\u017Eek 40 a\u017E 60 mm/hod, sklon 2 - 8\u00B0 a r\u016Fzn\u00E9 drsnosti p\u016Fdn\u00EDho povrchu). D\u00E1le popisuje stanovovan\u00E9 z\u00E1kladn\u00ED erozn\u00ED charakteristiky: mno\u017Estv\u00ED povrchov\u00E9ho odtoku, infiltrace, ztr\u00E1ty p\u016Fdy a dal\u0161\u00ED pro dosud testovan\u00E9zeminy: j\u00EDlovitohlinitou p\u016Fdu lokality Horom\u011B\u0159ice (testov\u00E1n\u00ED je dokon\u010Deno) a p\u00EDs\u010Ditohlinitou p\u016Fdu lokality T\u0159ebs\u00EDn. Z experiment\u00E1ln\u011B zji\u0161t\u011Bn\u00FDch dat je v\u017Edy kalkulov\u00E1na hodnota ust\u00E1len\u00E9 ztr\u00E1ty p\u016Fdy, kter\u00E1 ud\u00E1v\u00E1 tzv. erodovatelnost, tj. n\u00E1chylnost p\u016Fdy k erozi. Tato veli\u010Dina slou\u017E\u00ED jako vstupn\u00ED parametr do verifikace matematick\u00FDch simula\u010Dn\u00EDch model\u016F posuzuj\u00EDc\u00EDch sr\u00E1\u017Ekoodtokov\u00E9 vztahy a erozn\u00ED ohro\u017Een\u00ED v povod\u00EDch."@cs . "Vr\u00E1na, Karel" . . "Exactly determination of an amount of runoff, infiltration, runoff velocity, soil loss, etc. makes possible laboratory rainfall simulator of the Department of Irrigation, Drainage and Landscape Engineering, Faculty of Civil Engineering, CTU Prague. From obtained experiment values is calculated soil loss steady state value for different soil types. Rainfall intensity 40-60 mm per hour, slope 2-8\u00B0 and abrasiveness of soil surface were tested. Two soil types were the object of research to this time - clay-loam soil from Horom\u011B\u0159ice (testing is finished now) and sandy loam soil T\u0159ebs\u00EDn (experiments were starting for extreme dry conditions). We consider steady state value as an important indicator of erosion soil properties. We determine erodibility, e.g. soil immunity against erosion factors incidence, as input parameters to mathematics simulation models of rainfall-runoff relations from these values."@en . . "RIV/68407700:21110/05:01115196" . "Vesel\u00E1, Jana" . . . "[18F9E298BB28]" . . "21110" . . "80-01-03326-0" . "Erosion Characteristics Experimental Determination by Laboratory Rainfall Simulator"@en . . "Experiment\u00E1ln\u00ED stanovov\u00E1n\u00ED erozn\u00EDch charakteristik pomoc\u00ED laboratorn\u00EDho de\u0161\u0165ov\u00E9ho simul\u00E1toru"@cs . "Kole\u0161ka, Petr" . . . . "Erodibility; Mathematics Simulation Models; Rainfall Simulator; Soil Loss Properties; Surface Runoff; Water Erosion"@en . . . . . "Dost\u00E1l, Tom\u00E1\u0161" . "Vodn\u00ED hospod\u00E1\u0159stv\u00ED v krajin\u011B" . . "6"^^ . "7"^^ . . . "Erosion Characteristics Experimental Determination by Laboratory Rainfall Simulator"@en . "11"^^ . "Kol\u00E1\u010Dkov\u00E1, J." . . "161 ; 171" . . "521138" . "P(1P04OC634.001), Z(MSM6840770002)" . "\u010Cesk\u00E9 vysok\u00E9 u\u010Den\u00ED technick\u00E9 v Praze. Fakulta stavebn\u00ED" . . . . "Experiment\u00E1ln\u00ED stanovov\u00E1n\u00ED erozn\u00EDch charakteristik pomoc\u00ED laboratorn\u00EDho de\u0161\u0165ov\u00E9ho simul\u00E1toru" . . "RIV/68407700:21110/05:01115196!RIV07-MSM-21110___" . "\u010Cernice" . "Schwarzov\u00E1, Pavla" . "2005-09-13+02:00"^^ . . . "Experiment\u00E1ln\u00ED stanovov\u00E1n\u00ED erozn\u00EDch charakteristik pomoc\u00ED laboratorn\u00EDho de\u0161\u0165ov\u00E9ho simul\u00E1toru" . . "\u010Cl\u00E1nek popisuje Laboratorn\u00ED de\u0161\u0165ov\u00FD simul\u00E1tor Katedry hydromeliorac\u00ED a krajinn\u00E9ho in\u017Een\u00FDrstv\u00ED Fakulty stavebn\u00ED \u010CVUT Praha, princip prob\u00EDhaj\u00EDc\u00EDch experiment\u016F na n\u011Bm (pou\u017E\u00EDvan\u00E9 intenzity simulovan\u00FDch sr\u00E1\u017Eek 40 a\u017E 60 mm/hod, sklon 2 - 8\u00B0 a r\u016Fzn\u00E9 drsnosti p\u016Fdn\u00EDho povrchu). D\u00E1le popisuje stanovovan\u00E9 z\u00E1kladn\u00ED erozn\u00ED charakteristiky: mno\u017Estv\u00ED povrchov\u00E9ho odtoku, infiltrace, ztr\u00E1ty p\u016Fdy a dal\u0161\u00ED pro dosud testovan\u00E9zeminy: j\u00EDlovitohlinitou p\u016Fdu lokality Horom\u011B\u0159ice (testov\u00E1n\u00ED je dokon\u010Deno) a p\u00EDs\u010Ditohlinitou p\u016Fdu lokality T\u0159ebs\u00EDn. Z experiment\u00E1ln\u011B zji\u0161t\u011Bn\u00FDch dat je v\u017Edy kalkulov\u00E1na hodnota ust\u00E1len\u00E9 ztr\u00E1ty p\u016Fdy, kter\u00E1 ud\u00E1v\u00E1 tzv. erodovatelnost, tj. n\u00E1chylnost p\u016Fdy k erozi. Tato veli\u010Dina slou\u017E\u00ED jako vstupn\u00ED parametr do verifikace matematick\u00FDch simula\u010Dn\u00EDch model\u016F posuzuj\u00EDc\u00EDch sr\u00E1\u017Ekoodtokov\u00E9 vztahy a erozn\u00ED ohro\u017Een\u00ED v povod\u00EDch." . "Experiment\u00E1ln\u00ED stanovov\u00E1n\u00ED erozn\u00EDch charakteristik pomoc\u00ED laboratorn\u00EDho de\u0161\u0165ov\u00E9ho simul\u00E1toru"@cs . "Praha" . "Kavka, Petr" .