"Effect of Compacted Subsoil on Runoff Generation - Experimental Catchment Scale"@en . "RIV/68407700:21110/14:00220722!RIV15-GA0-21110___" . . . . "Vliv zhutn\u011Bl\u00E9ho podorni\u010D\u00ED na formov\u00E1n\u00ED podpovrchov\u00E9ho odtoku na m\u011B\u0159\u00EDtku experiment\u00E1ln\u00EDho povod\u00ED"@cs . "54005" . "Vliv zhutn\u011Bl\u00E9ho podorni\u010D\u00ED na formov\u00E1n\u00ED podpovrchov\u00E9ho odtoku na m\u011B\u0159\u00EDtku experiment\u00E1ln\u00EDho povod\u00ED" . . "P(GP13-20388P)" . . "Dost\u00E1l, Tom\u00E1\u0161" . . "The aim of the contribution is to examine the runoff dynamics along the inclined slope under different structural properties of the topsoil. We will present a numerical analysis of the effect of variable preferential domain ratio on subsurface runoff, the simulation results will be qualitatively compared to measured hydrographs at the catchment. We used a combination of physically based macroscopic models S1D and HYPO. In the S1D the dual permeability approach with two coupled Richards equations is used, the simultaneously operating HYPO code is based on a diffusion wave (Boussinesq eq.)."@en . "2"^^ . "Zumr, David" . . "ranfall; runoff; subsurface outflow; soil structure; soil compaction"@en . "2"^^ . . "21110" . . "Effect of Compacted Subsoil on Runoff Generation - Experimental Catchment Scale"@en . . . . . . "[7D8DB9959C10]" . "Vliv zhutn\u011Bl\u00E9ho podorni\u010D\u00ED na formov\u00E1n\u00ED podpovrchov\u00E9ho odtoku na m\u011B\u0159\u00EDtku experiment\u00E1ln\u00EDho povod\u00ED" . . "Aktu\u00E1ln\u00ED stav ornice na zem\u011Bd\u011Blsky obhospoda\u0159ovan\u00FDch ploch\u00E1ch ovliv\u0148uje mechanismus odtoku vody z povod\u00ED. Pokud je ornice kompaktn\u00ED, obsahuje pouze mal\u00E9 mno\u017Estv\u00ED makropor\u016F a m\u00E1 sn\u00ED\u017Eenou infiltra\u010Dn\u00ED kapacitu. Tento efekt je \u010Dasto umocn\u011Bn p\u016Fdn\u00ED krustou na povrchu. Za t\u011Bchto okolnost\u00ED doch\u00E1z\u00ED po intenzivn\u00EDch sr\u00E1\u017Ek\u00E1ch k formov\u00E1n\u00ED povrchov\u00E9ho odtoku. V obdob\u00ED po orb\u011B nebo podm\u00EDtce vykazuje ornice dobrou p\u016Fdn\u00ED strukturu, sr\u00E1\u017Ekov\u00E1 voda rychle infitruje meziagreg\u00E1tov\u00FDmi prostorami k m\u00E9n\u011B propustn\u00E9 vrstv\u011B v podorni\u010D\u00ED. Po t\u00E9to vrstv\u011B v reakci na vydatn\u00E9 sr\u00E1\u017Eky \u010D\u00E1st vody later\u00E1ln\u011B odt\u00E9k\u00E1. C\u00EDlem p\u0159\u00EDsp\u011Bvku je p\u0159edstavit konceptu\u00E1ln\u00ED model formov\u00E1n\u00ED podpovrchov\u00E9ho odtoku na p\u0159\u00EDkladu re\u00E1ln\u00FDch epizod zaznamenan\u00FDch na experiment\u00E1ln\u00EDm povod\u00ED Nu\u010Dice."@cs . "Aktu\u00E1ln\u00ED stav ornice na zem\u011Bd\u011Blsky obhospoda\u0159ovan\u00FDch ploch\u00E1ch ovliv\u0148uje mechanismus odtoku vody z povod\u00ED. Pokud je ornice kompaktn\u00ED, obsahuje pouze mal\u00E9 mno\u017Estv\u00ED makropor\u016F a m\u00E1 sn\u00ED\u017Eenou infiltra\u010Dn\u00ED kapacitu. Tento efekt je \u010Dasto umocn\u011Bn p\u016Fdn\u00ED krustou na povrchu. Za t\u011Bchto okolnost\u00ED doch\u00E1z\u00ED po intenzivn\u00EDch sr\u00E1\u017Ek\u00E1ch k formov\u00E1n\u00ED povrchov\u00E9ho odtoku. V obdob\u00ED po orb\u011B nebo podm\u00EDtce vykazuje ornice dobrou p\u016Fdn\u00ED strukturu, sr\u00E1\u017Ekov\u00E1 voda rychle infitruje meziagreg\u00E1tov\u00FDmi prostorami k m\u00E9n\u011B propustn\u00E9 vrstv\u011B v podorni\u010D\u00ED. Po t\u00E9to vrstv\u011B v reakci na vydatn\u00E9 sr\u00E1\u017Eky \u010D\u00E1st vody later\u00E1ln\u011B odt\u00E9k\u00E1. C\u00EDlem p\u0159\u00EDsp\u011Bvku je p\u0159edstavit konceptu\u00E1ln\u00ED model formov\u00E1n\u00ED podpovrchov\u00E9ho odtoku na p\u0159\u00EDkladu re\u00E1ln\u00FDch epizod zaznamenan\u00FDch na experiment\u00E1ln\u00EDm povod\u00ED Nu\u010Dice." . . . "RIV/68407700:21110/14:00220722" . "Vliv zhutn\u011Bl\u00E9ho podorni\u010D\u00ED na formov\u00E1n\u00ED podpovrchov\u00E9ho odtoku na m\u011B\u0159\u00EDtku experiment\u00E1ln\u00EDho povod\u00ED"@cs . .