. "Vodn\u00ED re\u017Eim v lesn\u00EDm povod\u00ED %22U Dvou lou\u010Dek%22 v Orlick\u00FDch hor\u00E1ch je ovl\u00E1d\u00E1n vodn\u00EDm re\u017Eimem typ\u016F p\u016Fd. Vodn\u00ED re\u017Eim humusov\u00FDch podzol\u016F vykazuje vy\u0161\u0161\u00ED objem ob\u011Bhu gravita\u010Dn\u00ED vody k objemu vody kapil\u00E1rn\u00ED a semikapil\u00E1rn\u00ED ne\u017E kambizem\u011B. P\u0159\u00ED\u010Dinou jsou odchyln\u00E9 hydropedologick\u00E9 vlastnosti obou typ\u016F lesn\u00EDch p\u016Fd. K \u0159e\u0161en\u00ED byla zvolena metoda hydrologick\u00E9 bilance, kterou se poda\u0159ilo objasnit \u00FAlohu gravita\u010Dn\u00EDch a kapil\u00E1rn\u00EDch a semikapil\u00E1rn\u00EDch vod v aera\u010Dn\u00ED z\u00F3n\u011B lesn\u00EDch p\u016Fd vrcholn\u00FDch parti\u00ED Orlick\u00FDch hor." . "RIV/00020702:_____/11:#0000572" . "Hydrologick\u00E1 bilance v lesn\u00EDm horsk\u00E9m povod\u00ED dle p\u016Fdn\u00EDch typ\u016F" . . . . . "Vodn\u00ED re\u017Eim v lesn\u00EDm povod\u00ED %22U Dvou lou\u010Dek%22 v Orlick\u00FDch hor\u00E1ch je ovl\u00E1d\u00E1n vodn\u00EDm re\u017Eimem typ\u016F p\u016Fd. Vodn\u00ED re\u017Eim humusov\u00FDch podzol\u016F vykazuje vy\u0161\u0161\u00ED objem ob\u011Bhu gravita\u010Dn\u00ED vody k objemu vody kapil\u00E1rn\u00ED a semikapil\u00E1rn\u00ED ne\u017E kambizem\u011B. P\u0159\u00ED\u010Dinou jsou odchyln\u00E9 hydropedologick\u00E9 vlastnosti obou typ\u016F lesn\u00EDch p\u016Fd. K \u0159e\u0161en\u00ED byla zvolena metoda hydrologick\u00E9 bilance, kterou se poda\u0159ilo objasnit \u00FAlohu gravita\u010Dn\u00EDch a kapil\u00E1rn\u00EDch a semikapil\u00E1rn\u00EDch vod v aera\u010Dn\u00ED z\u00F3n\u011B lesn\u00EDch p\u016Fd vrcholn\u00FDch parti\u00ED Orlick\u00FDch hor."@cs . . . "Hydrologick\u00E1 bilance v lesn\u00EDm horsk\u00E9m povod\u00ED dle p\u016Fdn\u00EDch typ\u016F"@cs . . . . . . . "RIV/00020702:_____/11:#0000572!RIV12-MZE-00020702" . "forest catchment; soils; hydrology"@en . . "Hydrological balance in forest mountain catchment according to forest soil classes"@en . "Water regime in the %22U Dvou lou\u010Dek%22 forest catchment in the Orlick\u00E9 hory Mts. is under the influence of water regime of forest soil classes. Water regime of humus podzols performs higher volume of gravitational water cicrulation to volume of capilar and semicapilar water than cambisol. The reason are different hydropedological characteristics of both soil classes. To solve that, we chose the method of hydrological balance."@en . "203139" . . "[14D1B8FE9FFE]" . "Hydrologick\u00E1 bilance v lesn\u00EDm horsk\u00E9m povod\u00ED dle p\u016Fdn\u00EDch typ\u016F" . "3"^^ . . "Hydrological balance in forest mountain catchment according to forest soil classes"@en . . "P(QH92073), P(QI112A174), Z(MZE0002070203)" . . . "Hydrologick\u00E1 bilance v lesn\u00EDm horsk\u00E9m povod\u00ED dle p\u016Fdn\u00EDch typ\u016F"@cs . "\u0160ach, Franti\u0161ek" . "2"^^ . "\u0160vihla, Vladim\u00EDr" . "\u010Cernohous, Vladim\u00EDr" . .