"20. vyd., Brno" . "\u0160imkov\u00E1, Pavl\u00EDna" . "The soil environment and biological activity in the forest soils of the mountain area national natural reservation \u010Cert\u016Fv ml\u00FDn, Moravian-Silesian Beskids"@en . "4"^^ . "Vav\u0159\u00ED\u010Dek, Du\u0161an" . . . . . "8"^^ . "humus; Haplic Podzol; sandstone bedrock; forest tree composition; catalase"@en . . . . "The Moravian-Silesian Beskids (Czech Republic) are situated in the northwestern section of the Extend Western Carpatians characteristics. The isolated peaks with unusual sites heterogeneity and biodiversity (e.g. massif Kn\u011Bhyn\u011B-\u010Cert\u016Fv Ml\u00FDn) can be found there. Those sites were tectonically affected and it resulted to several ways of the physics weathering such as pseudo-karst. Podzolization is generally caused by sandstone substrate texture in connection with cold humid mountain climate (+4.8oC, 1,190 mm).Differential subsoil weathering and shift events affected significantly diversity of the humus forms as well as small-area spread of the forest types. The representative sites of the mountain fir-beech-spruce forest (association Calamagrostio-villosae Fagetum/Picetum) were selected. The sites on Kn\u011Bhyn\u011B Mt. were located in the natural spruce (Picea abies (L.) Karsten) forests upon 1000 m a.s.l. The sites on \u010Cert\u016Fv ml\u00FDn Mt. were located in the mixed allochthonous mountain forests at the altitude 930 -" . . "109;116" . . "The soil environment and biological activity in the forest soils of the mountain area national natural reservation \u010Cert\u016Fv ml\u00FDn, Moravian-Silesian Beskids" . "978-80-7375-069-5" . "The Moravian-Silesian Beskids (Czech Republic) are situated in the northwestern section of the Extend Western Carpatians characteristics. The isolated peaks with unusual sites heterogeneity and biodiversity (e.g. massif Kn\u011Bhyn\u011B-\u010Cert\u016Fv Ml\u00FDn) can be found there. Those sites were tectonically affected and it resulted to several ways of the physics weathering such as pseudo-karst. Podzolization is generally caused by sandstone substrate texture in connection with cold humid mountain climate (+4.8oC, 1,190 mm).Differential subsoil weathering and shift events affected significantly diversity of the humus forms as well as small-area spread of the forest types. The representative sites of the mountain fir-beech-spruce forest (association Calamagrostio-villosae Fagetum/Picetum) were selected. The sites on Kn\u011Bhyn\u011B Mt. were located in the natural spruce (Picea abies (L.) Karsten) forests upon 1000 m a.s.l. The sites on \u010Cert\u016Fv ml\u00FDn Mt. were located in the mixed allochthonous mountain forests at the altitude 930 -"@en . "P\u016Fdn\u00ED prost\u0159ed\u00ED a biologick\u00E1 aktivita lesn\u00EDch p\u016Fd v horsk\u00E9 oblasti NPR \u010Cert\u016Fv ml\u00FDn, Moravskoslezsk\u00E9 Beskydy"@cs . "43410" . "Mendelova zem\u011Bd\u011Blsk\u00E1 a lesnick\u00E1 univerzita v Brn\u011B. Lesnick\u00E1 a d\u0159eva\u0159sk\u00E1 fakulta" . . "The soil environment and biological activity in the forest soils of the mountain area national natural reservation \u010Cert\u016Fv ml\u00FDn, Moravian-Silesian Beskids" . "Samec, Pavel" . "Beskydy" . "Form\u00E1nek, Pavel" . . "450887" . . . . "RIV/62156489:43410/07:00110011!RIV08-MSM-43410___" . . "P\u016Fdn\u00ED prost\u0159ed\u00ED a biologick\u00E1 aktivita lesn\u00EDch p\u016Fd v horsk\u00E9 oblasti NPR \u010Cert\u016Fv ml\u00FDn, Moravskoslezsk\u00E9 Beskydy"@cs . "Z(MSM6215648902)" . . . "[E01A073A4180]" . "The soil environment and biological activity in the forest soils of the mountain area national natural reservation \u010Cert\u016Fv ml\u00FDn, Moravian-Silesian Beskids"@en . . "Moravskoslezsk\u00E9 Beskydy se nach\u00E1zej\u00ED v severoz\u00E1pan\u00ED \u010D\u00E1sti z\u00E1padn\u00EDch Karpat. Nach\u00E1zej\u00ED se tu izolovan\u00E9 vrcholy s neobvyklou heterogenitou a biodiversitou (nap\u0159. mas\u00EDv Kn\u011Bhyn\u011B - \u010Cert\u016Fv ml\u00FDn). R\u016Fzn\u00E9 typy zv\u011Btr\u00E1v\u00E1n\u00ED na t\u011Bchto tektonicky ovlivn\u011Bn\u00FDch lokalit\u00E1ch vedlo k vzniku pseudokrasu. Podzolizace se b\u011B\u017En\u011B objevuje na p\u00EDs\u010Dit\u00FDch substr\u00E1tech ve spojen\u00ED s chlad\u00FDm a vlhk\u00FDm horsk\u00FDm klimatem (+4.8oC, 1,190 mm). Rozd\u00EDln\u00E9 zv\u011Btr\u00E1v\u00E1n\u00ED podlo\u017E\u00ED v\u00FDznamn\u011B ovlivnilo humusov\u00E9 formy stejn\u011B jako rozt\u0159\u00ED\u0161t\u011Bnost lesn\u00EDch typ\u016F. Na lokalit\u011B byly vybr\u00E1ny plochy v asociaci Calamagrostio-villosae Fagetum/Picetum. Plochy na lokalit\u011B Kn\u011Bhyn\u011B reprezentuj\u00ED p\u0159irozen\u00FD smrkov\u00FD les (Picea abies (L.) Karsten) do 1000 m n.m. Plochy na lokalit\u011B \u010Cert\u016Fv ml\u00FDn se nach\u00E1zej\u00ED ve sm\u00ED\u0161en\u00E9m alochtonn\u00EDm horsk\u00E9m lese v nadmo\u0159sk\u00E9 v\u00FDs\u0161ce 930 - 960 m. Aktivita p\u016Fdn\u00ED katal\u00E1zy, pH, oxidovateln\u00FD uhl\u00EDk, celkov\u00FD dus\u00EDk a humusov\u00E9 l\u00E1tky z horizont\u016F H a Ae/Ep byly hodnoceny na podzim 2005 a 2006. Z\u00EDskan\u00E1 data byla porovn\u00E1na anal\u00FDzou hlavn\u00EDch komponent\u016F (PCA). Rozd"@cs . "4"^^ . "RIV/62156489:43410/07:00110011" . . .