. . "SK - Slovensk\u00E1 republika" . . . . . "Vliv p\u016Fdn\u00EDho profilu na sr\u00E1\u017Ekoodtokov\u00FD proces"@cs . "Nov\u00E1k, Luk\u00E1\u0161" . "P(IBS2060104), P(SA/650/5/03)" . "V Jizersk\u00FDch hor\u00E1ch na povod\u00ED Uhl\u00ED\u0159sk\u00E1 prob\u00EDh\u00E1 hydrologick\u00E9 monitorov\u00E1n\u00ED zam\u011B\u0159en\u00E9 na sledov\u00E1n\u00ED proces\u016F vodn\u00ED bilance p\u016Fdn\u00EDho profilu. P\u016Fdn\u00ED profil, tvo\u0159en\u00FD hn\u011Bdou p\u016Fdou kyselou (Dystric Cambisol), je m\u011Blk\u00FD a vysoce heterogenn\u00ED, formovan\u00FD na zv\u011Btral\u00E9m \u017Eulov\u00E9m podlo\u017E\u00ED. B\u011Bhem sedmi vegeta\u010Dn\u00EDch obdob\u00ED bylo zaznamen\u00E1no v\u00EDce ne\u017E 25 v\u00FDznamn\u00FDch odtokov\u00FDch ud\u00E1lost\u00ED, zp\u016Fsoben\u00FDch infiltrac\u00ED sr\u00E1\u017Eek r\u016Fzn\u00FDch intenzit a dob trv\u00E1n\u00ED. Odtokov\u00E9 jevy vykazuj\u00ED vysokou m\u00EDru variability vztahu p\u016Fdn\u00EDho sac\u00EDho tlaku, p\u016Fdn\u00ED vlhkosti v\u016F\u010Di okam\u017Eit\u00E9 intenzit\u011B odtoku. Moment\u00E1ln\u00ED vlhkost p\u016Fdn\u00EDho profilu z\u00E1vis\u00ED na historii pln\u011Bn\u00ED p\u00F3rov\u00E9ho prostoru. P\u016Fdn\u00ED profil je p\u0159ev\u00E1\u017En\u011B nenasycen\u00FD, p\u0159esto je po v\u011Bt\u0161inu \u010Dasu bl\u00EDzko nasycen\u00ED, co\u017E ovliv\u0148uje pr\u016Fb\u011Bh podpovrchov\u00E9ho odtoku. Vztah v\u00FD\u0161ky hladiny podzemn\u00ED vody, p\u016Fdn\u00ED vlhkosti a podpovrchov\u00E9ho odtoku s celkov\u00FDm odtokem z povod\u00ED je velmi t\u011Bsn\u00FD."@cs . . "21110" . . . . "C\u00EDslerov\u00E1, Milena" . . . "Vliv p\u016Fdn\u00EDho profilu na sr\u00E1\u017Ekoodtokov\u00FD proces"@cs . "V Jizersk\u00FDch hor\u00E1ch na povod\u00ED Uhl\u00ED\u0159sk\u00E1 prob\u00EDh\u00E1 hydrologick\u00E9 monitorov\u00E1n\u00ED zam\u011B\u0159en\u00E9 na sledov\u00E1n\u00ED proces\u016F vodn\u00ED bilance p\u016Fdn\u00EDho profilu. P\u016Fdn\u00ED profil, tvo\u0159en\u00FD hn\u011Bdou p\u016Fdou kyselou (Dystric Cambisol), je m\u011Blk\u00FD a vysoce heterogenn\u00ED, formovan\u00FD na zv\u011Btral\u00E9m \u017Eulov\u00E9m podlo\u017E\u00ED. B\u011Bhem sedmi vegeta\u010Dn\u00EDch obdob\u00ED bylo zaznamen\u00E1no v\u00EDce ne\u017E 25 v\u00FDznamn\u00FDch odtokov\u00FDch ud\u00E1lost\u00ED, zp\u016Fsoben\u00FDch infiltrac\u00ED sr\u00E1\u017Eek r\u016Fzn\u00FDch intenzit a dob trv\u00E1n\u00ED. Odtokov\u00E9 jevy vykazuj\u00ED vysokou m\u00EDru variability vztahu p\u016Fdn\u00EDho sac\u00EDho tlaku, p\u016Fdn\u00ED vlhkosti v\u016F\u010Di okam\u017Eit\u00E9 intenzit\u011B odtoku. Moment\u00E1ln\u00ED vlhkost p\u016Fdn\u00EDho profilu z\u00E1vis\u00ED na historii pln\u011Bn\u00ED p\u00F3rov\u00E9ho prostoru. P\u016Fdn\u00ED profil je p\u0159ev\u00E1\u017En\u011B nenasycen\u00FD, p\u0159esto je po v\u011Bt\u0161inu \u010Dasu bl\u00EDzko nasycen\u00ED, co\u017E ovliv\u0148uje pr\u016Fb\u011Bh podpovrchov\u00E9ho odtoku. Vztah v\u00FD\u0161ky hladiny podzemn\u00ED vody, p\u016Fdn\u00ED vlhkosti a podpovrchov\u00E9ho odtoku s celkov\u00FDm odtokem z povod\u00ED je velmi t\u011Bsn\u00FD." . . "Journal of Hydrology and Hydromechanics" . "Impact of the soil profile on the rainfall-runoff process"@en . "54" . "4"^^ . . "Impact of the soil profile on the rainfall-runoff process"@en . . "506707" . "4"^^ . "2" . . "The experimental watershed Uhl\u00ED\u0159sk\u00E1 hydrological monitoring on the continual basis focused towards the processes of water balance in the soil profile. The typical soil profile is highly heterogeneous, formed by 0.8-1.2 m of Cambisols based on the decayed and fractured granite bedrock. At the locality Tom\u0161ovka, the experimental hillslope transect has been instrumented. In the subsurface trench, subsurface outflow is monitored and soil water suction is scanned by tensiometers adjacent to the trench. During seven vegetation periods more than 25 significant runoff events has been recorded. They are caused by a rainfall of a different intensity and duration. Runoff behaviour is of a high variability in terms of soil suction, soil moisture or depth of water in the soil profile in the vicinity of the trench. Instant moisture in the soil profile depends on the history of filling of the pore space."@en . "[C8DD649CE258]" . "Vliv p\u016Fdn\u00EDho profilu na sr\u00E1\u017Ekoodtokov\u00FD proces" . . "\u0160anda, Martin" . "Hrn\u010D\u00ED\u0159, Miroslav" . "RIV/68407700:21110/06:01125954!RIV07-MZP-21110___" . "9"^^ . "Vliv p\u016Fdn\u00EDho profilu na sr\u00E1\u017Ekoodtokov\u00FD proces" . . "RIV/68407700:21110/06:01125954" . "183;191" . "0042-790X" . . . "Crystalline bedrock; Hillslope; Rainfall; Runoff; Soil profile; Watershed"@en . . .