. "RIV/62156489:43410/08:00134105!RIV09-MSM-43410___" . . "\u010CZU v Praze, \u00DAH\u00DAL Brand\u00FDs nad Labem" . "Vodohospod\u00E1\u0159sk\u00E9 funkce les\u016F v krajin\u011B maj\u00ED zcela nezastupitelnou roli pro udr\u017Een\u00ED vodn\u00EDch potenci\u00E1l\u016F. V \u00FAvalov\u00FDch reli\u00E9fech jsou vodohospod\u00E1\u0159sky nejd\u016Fle\u017Eit\u011Bj\u0161\u00ED lu\u017En\u00ED lesy. V odlesn\u011Bn\u00E9 krajin\u011B se v\u017Edy nebezpe\u010Dn\u011B projevuje eroze i sez\u00F3nn\u00ED prosych\u00E1n\u00ED obna\u017Een\u00FDch substr\u00E1t\u016F. Po\u0159\u00EDzen\u00E9 v\u00FDsledky stanoven\u00ED potenci\u00E1ln\u00EDch reten\u010Dn\u00EDch vodn\u00EDch kapacit p\u0159evl\u00E1daj\u00EDc\u00EDch p\u016Fdn\u00EDch typ\u016F poukazuj\u00ED na celkov\u00E9 mno\u017Estv\u00ED vody, kter\u00E9 m\u016F\u017Ee objem dan\u00E9ho pedonu zadr\u017Eet po dobu 24 hod. V\u00FDsledky stanoven\u00ED efektivn\u00EDch reten\u010Dn\u00EDch vodn\u00EDch kapacit lesn\u00EDch p\u016Fd upom\u00EDnaj\u00ED na skute\u010Dn\u00FD objem kapil\u00E1rn\u011B v\u00E1zan\u00E9 vody v lesn\u00ED p\u016Fd\u011B, dostupn\u00E9 pro transpiraci. P\u0159\u00EDm\u00FD vztah t\u011Bchto charakteristik s potenci\u00E1ln\u00ED retardac\u00ED nadlimitn\u00EDch odtok\u016F nen\u00ED pr\u016Fkazn\u00FD, av\u0161ak nep\u0159\u00EDmo indikuje oblasti s v\u00FDznamnou kapilaritou a oblasti s n\u00EDzkou kapilaritou lesn\u00EDch p\u016Fd, n\u00E1chyln\u00FDch v\u016F\u010Di suchu, resp. z\u00E1visl\u00FDch na dod\u00E1vk\u00E1ch podzemn\u00ED nebo \u0159\u00ED\u010Dn\u00ED vody. Charakteristick\u00E1 distribuce RVKef nazna\u010Duje, \u017Ee p\u0159edev\u0161\u00EDm vodou neovlivn\u011Bn\u00E9 p\u016Fdy v pahorkatinn\u00FDch a\u017E horsk\u00FDch oblastech jsou" . . "[562BEF2DEF64]" . "Povodn\u011B a hydrick\u00E9 potenci\u00E1ly lesn\u00EDch p\u016Fd v Moravskoslezsk\u00E9m kraji"@cs . "RIV/62156489:43410/08:00134105" . "43410" . "Vodohospod\u00E1\u0159sk\u00E9 funkce les\u016F v krajin\u011B maj\u00ED zcela nezastupitelnou roli pro udr\u017Een\u00ED vodn\u00EDch potenci\u00E1l\u016F. V \u00FAvalov\u00FDch reli\u00E9fech jsou vodohospod\u00E1\u0159sky nejd\u016Fle\u017Eit\u011Bj\u0161\u00ED lu\u017En\u00ED lesy. V odlesn\u011Bn\u00E9 krajin\u011B se v\u017Edy nebezpe\u010Dn\u011B projevuje eroze i sez\u00F3nn\u00ED prosych\u00E1n\u00ED obna\u017Een\u00FDch substr\u00E1t\u016F. Po\u0159\u00EDzen\u00E9 v\u00FDsledky stanoven\u00ED potenci\u00E1ln\u00EDch reten\u010Dn\u00EDch vodn\u00EDch kapacit p\u0159evl\u00E1daj\u00EDc\u00EDch p\u016Fdn\u00EDch typ\u016F poukazuj\u00ED na celkov\u00E9 mno\u017Estv\u00ED vody, kter\u00E9 m\u016F\u017Ee objem dan\u00E9ho pedonu zadr\u017Eet po dobu 24 hod. V\u00FDsledky stanoven\u00ED efektivn\u00EDch reten\u010Dn\u00EDch vodn\u00EDch kapacit lesn\u00EDch p\u016Fd upom\u00EDnaj\u00ED na skute\u010Dn\u00FD objem kapil\u00E1rn\u011B v\u00E1zan\u00E9 vody v lesn\u00ED p\u016Fd\u011B, dostupn\u00E9 pro transpiraci. P\u0159\u00EDm\u00FD vztah t\u011Bchto charakteristik s potenci\u00E1ln\u00ED retardac\u00ED nadlimitn\u00EDch odtok\u016F nen\u00ED pr\u016Fkazn\u00FD, av\u0161ak nep\u0159\u00EDmo indikuje oblasti s v\u00FDznamnou kapilaritou a oblasti s n\u00EDzkou kapilaritou lesn\u00EDch p\u016Fd, n\u00E1chyln\u00FDch v\u016F\u010Di suchu, resp. z\u00E1visl\u00FDch na dod\u00E1vk\u00E1ch podzemn\u00ED nebo \u0159\u00ED\u010Dn\u00ED vody. Charakteristick\u00E1 distribuce RVKef nazna\u010Duje, \u017Ee p\u0159edev\u0161\u00EDm vodou neovlivn\u011Bn\u00E9 p\u016Fdy v pahorkatinn\u00FDch a\u017E horsk\u00FDch oblastech jsou"@cs . . . . "388241" . "soil retention; capilarity; forest soil"@en . . "Z(MSM6215648902)" . "The hydric function of forests in environment creates important role for sustainability of hydric potentials.In lowlands are most important forests. In clear felled areas attend to erosion processes and seasonal drying of topsoil horizons. Received results of potential retention capacities prevailing soil types display total amounth of water, which can certain value of soil keep during 24 hours. The result of efevtive retentional water capacities for forest soils express real value of hold water in forest soil, usable for transpiration. The direct relation of these characteristics with potential retardation is not visible, but induces areas with significant capilarity and and areas with low capilarity of forest soil, sensitive to dryspells, depended on supply due to underground or river water.Characteristical disturbance express, that expecially water unifluenced soil from lowlands to mountanious areas are relatively resistant to dryspells, while fluvisoils and semihydromorphic soils has availability"@en . . . . . "978-80-213-1841-0" . "Povodn\u011B a hydrick\u00E9 potenci\u00E1ly lesn\u00EDch p\u016Fd v Moravskoslezsk\u00E9m kraji" . . "Floods and hydrical potentials of forest soil in Moravian-silesian area"@en . "Vav\u0159\u00ED\u010Dek, Du\u0161an" . "Samec, Pavel" . "Zm\u011Bny klimatu a lesnictv\u00ED" . . "34"^^ . . "142"^^ . "Praha" . . "Floods and hydrical potentials of forest soil in Moravian-silesian area"@en . "3"^^ . . . "Povodn\u011B a hydrick\u00E9 potenci\u00E1ly lesn\u00EDch p\u016Fd v Moravskoslezsk\u00E9m kraji"@cs . "Ku\u010Dera, Ale\u0161" . "3"^^ . "Povodn\u011B a hydrick\u00E9 potenci\u00E1ly lesn\u00EDch p\u016Fd v Moravskoslezsk\u00E9m kraji" .