"Possibilities of forests in reducing floods"@en . . "Mo\u017Enosti les\u016F p\u0159i tlumen\u00ED povodn\u00ED"@cs . . "St\u0159edohorsk\u00E9 a horsk\u00E9 lesy (na rozd\u00EDl od v\u0161ech nelesn\u00EDch ekosyst\u00E9m\u016F) tlum\u00ED velmi snadno p\u0159\u00EDvalov\u00E9 sr\u00E1\u017Eky o s\u00EDle do 50 mm. Souvisl\u00E9 sr\u00E1\u017Eky o velikosti do 100 mm se ji\u017E projev\u00ED na celkov\u00E9 v\u00FD\u0161i odtoku vody z lesa, ale z pohledu vodohospod\u00E1\u0159sk\u00E9 \u00FA\u010Dinnosti jsou je\u0161t\u011B p\u0159ijateln\u00E9. Za kritickou mez pro \u00FA\u010Dinn\u00E9 tlumen\u00ED povodn\u00ED lesem lze pova\u017Eovat hranici 150 a\u017E 200 mm souvisl\u00FDch sr\u00E1\u017Eek. P\u0159i tomto \u00FAhrnu je ji\u017E lesn\u00ED p\u016Fda v\u017Edy zcela nasycena vodou v\u010Detn\u011B zapln\u011Bn\u00ED prohlubn\u00ED jak v p\u016Fdn\u00EDm povrchu, tak v horninov\u00E9m podlo\u017E\u00ED. Pot\u00E9 nast\u00E1v\u00E1 ne\u0159\u00EDzen\u00FD a spont\u00E1nn\u00ED odtok vody cel\u00FDm p\u016Fdn\u00EDm profilem, vystupuj\u00EDc\u00ED \u010Dasto i na povrch p\u016Fdy, a to bez ohledu na druhovou skladbu nebo sebejemn\u011Bj\u0161\u00ED zp\u016Fsoby obhospoda\u0159ov\u00E1n\u00ED."@cs . . "81" . "St\u0159edohorsk\u00E9 a horsk\u00E9 lesy (na rozd\u00EDl od v\u0161ech nelesn\u00EDch ekosyst\u00E9m\u016F) tlum\u00ED velmi snadno p\u0159\u00EDvalov\u00E9 sr\u00E1\u017Eky o s\u00EDle do 50 mm. Souvisl\u00E9 sr\u00E1\u017Eky o velikosti do 100 mm se ji\u017E projev\u00ED na celkov\u00E9 v\u00FD\u0161i odtoku vody z lesa, ale z pohledu vodohospod\u00E1\u0159sk\u00E9 \u00FA\u010Dinnosti jsou je\u0161t\u011B p\u0159ijateln\u00E9. Za kritickou mez pro \u00FA\u010Dinn\u00E9 tlumen\u00ED povodn\u00ED lesem lze pova\u017Eovat hranici 150 a\u017E 200 mm souvisl\u00FDch sr\u00E1\u017Eek. P\u0159i tomto \u00FAhrnu je ji\u017E lesn\u00ED p\u016Fda v\u017Edy zcela nasycena vodou v\u010Detn\u011B zapln\u011Bn\u00ED prohlubn\u00ED jak v p\u016Fdn\u00EDm povrchu, tak v horninov\u00E9m podlo\u017E\u00ED. Pot\u00E9 nast\u00E1v\u00E1 ne\u0159\u00EDzen\u00FD a spont\u00E1nn\u00ED odtok vody cel\u00FDm p\u016Fdn\u00EDm profilem, vystupuj\u00EDc\u00ED \u010Dasto i na povrch p\u016Fdy, a to bez ohledu na druhovou skladbu nebo sebejemn\u011Bj\u0161\u00ED zp\u016Fsoby obhospoda\u0159ov\u00E1n\u00ED." . "P(GA526/02/0851), Z(MSM 434100005), Z(MZE-M06-99-01)" . "Mid-mountain and mountain forests (in contrast to all non-forest ecosystems) mitigate very easily rainstorms of up to a 50 mm intensity. Continuos precipitation up to 100 mm can be already shown in the total amount of runoff from the forest; however, from the viewpoint of water-management effectiveness they are acceptable. A limit of 150 to 200 mm continuous precipitation can be considered to be a critical boundary for the effective mitigation of floods by the forest. Under conditions of the precipitation total, forest soil is always completely saturated by water including filling up depressions both in the soil surface and in the subsoil. Then, uncontrolled and spontaneous runoff occurs through the whole soil profile appearing often even on the soil surface regardless of the species composition or anywise sophisticated methods of forest management."@en . . "RIV/62156489:_____/02:42600010" . "water regime; beech; floods; mountain forests; norway spruce"@en . "3"^^ . . . "\u0160ach, Franti\u0161ek" . "Kantor, Petr" . . . "0322-9254" . "Mo\u017Enosti les\u016F p\u0159i tlumen\u00ED povodn\u00ED" . "CZ - \u010Cesk\u00E1 republika" . . . "Mo\u017Enosti les\u016F p\u0159i tlumen\u00ED povodn\u00ED"@cs . "654412" . "Possibilities of forests in reducing floods"@en . "1"^^ . . "[50CF39495473]" . . . "Mo\u017Enosti les\u016F p\u0159i tlumen\u00ED povodn\u00ED" . "Lesnick\u00E1 pr\u00E1ce : \u010Dasopis pro lesnickou v\u011Bdu a praxi" . . "11" . . . . . "2"^^ . "RIV/62156489:_____/02:42600010!RIV09-GA0-62156489" . . .