"552376" . . "Zm\u011Bny vlastnost\u00ED p\u016Fdy p\u0159i bezorebn\u00E9m zpracov\u00E1n\u00ED v rozd\u00EDln\u00FDch p\u016Fdn\u011B -klimatick\u00FDch podm\u00EDnk\u00E1ch"@cs . . . "12220" . "P(1G57042), Z(MSM6007665806)" . "Ochrana a vyu\u017Eit\u00ED p\u016Fdy v podhorsk\u00FDch oblastech : sborn\u00EDk v\u011Bdeck\u00FDch prac\u00ED, 1.-2. z\u00E1\u0159\u00ED 2005, Nov\u00E9 Hrady" . . "Changes of soil properties under minimum tillage in different soil-climatic conditions"@en . "In a precise large - plot (Gross Enzerdorf - GE - chernozem) and a medium-term operational (Stagra Studen\u00E1 - ST - cambisol) trials, chosen physical - chemical properties of soil have been observed, at comparison of %22minimum tillage%22 (MT) and %22conventional tillage%22 (CT) technologies of its cultivation in three depths of soil profile in spring (S) and autumn (O). Soil moisture conditions, bulk density (Or) and compaction level (MPa) at cambisol were more favourable at CT in the depth to 0,2 m, in the depth of 0,25 - 0,3 m the values were already comparable at both technologies or slinghtly more favourable at MT. At chernozem on the contrary, soil moisture conditions in coarse of year were better at MT in the whole profile. Bulk density was here to the depth of 0,3 m at MT more uniform, but insifignicantly higher than at CT (O 1,29 g.cm-3), and to the depth of 0,5 m is decreasing to O 1,15 g.m-3 . At CT, it is increasing in the depth 0,3 - 0,4 m even to 1,37 g.cm-3. Average contents o"@en . "Zm\u011Bny vlastnost\u00ED p\u016Fdy p\u0159i bezorebn\u00E9m zpracov\u00E1n\u00ED v rozd\u00EDln\u00FDch p\u016Fdn\u011B -klimatick\u00FDch podm\u00EDnk\u00E1ch"@cs . . "minimum tillage; soil physical properties; humus content and quality"@en . "7"^^ . "\u010Cechov\u00E1, V\u011Bra" . "Ledvina, Rostislav" . "2005-09-01+02:00"^^ . . "Zm\u011Bny vlastnost\u00ED p\u016Fdy p\u0159i bezorebn\u00E9m zpracov\u00E1n\u00ED v rozd\u00EDln\u00FDch p\u016Fdn\u011B -klimatick\u00FDch podm\u00EDnk\u00E1ch" . "RIV/60076658:12220/05:00006247!RIV06-MZE-12220___" . "\u010Cesk\u00E9 Bud\u011Bjovice" . . "Hor\u00E1\u010Dek, Jan" . . . . . . "3"^^ . . . "Jiho\u010Desk\u00E1 univerzita v \u010Cesk\u00FDch Bud\u011Bjovic\u00EDch. Zem\u011Bd\u011Blsk\u00E1 fakulta" . . "3"^^ . "V p\u0159esn\u00E9m velkoparcelkov\u00E9m (\u010Dernozem - Gross Enzerdorf) a st\u0159edn\u011Bdob\u00E9m provozn\u00EDm (kambizem - Stagra Studen\u00E1) pokusu jsou sledov\u00E1ny vybran\u00E9 fyzik\u00E1ln\u011B chemick\u00E9 vlastnosti p\u016Fdy p\u0159i porovn\u00E1n\u00ED bezorebn\u00E9 (MT( a konven\u010Dn\u00ED (CT) technologie technologie jej\u00EDho zpracov\u00E1n\u00ED v p\u016Fdn\u00EDm profilu na ja\u0159e a na podzim. Fyzik\u00E1ln\u00ED parametry p\u016Fdy byly u kambizem\u011B p\u0159\u00EDzniv\u011Bj\u0161\u00ED u CT v hloubce 0,2 m, v hloubce 0,25 - 0,30 m byly ji\u017E hodnoty srovnateln\u00E9 nebo m\u00EDrn\u011B p\u0159\u00EDzniv\u011Bj\u0161\u00ED u MT. U \u010Dernozem\u011B byly naopak vlhkostn\u00ED pom\u011Bry v pr\u016Fb\u011Bhuroku lep\u0161\u00ED u MT v cel\u00E9m p\u016Fdn\u00EDm profilu. Or zde byla do hloubky 0,3 m u MT rovnom\u011Brn\u011Bj\u0161\u00ED ,ale nepatrn\u011B vy\u0161\u0161\u00ED ne\u017E v CT a do hloubky 0,5 m se sni\u017Euje. U CT doch\u00E1z\u00ED v hloubce 0,3 - 0,4 m naopak k jej\u00EDmu zv\u00FD\u0161en\u00ED. Pr\u016Fm\u011Brn\u00E9 obsahy celkov\u00E9ho uhl\u00EDku (Cox) byly ukambizem\u011B v hloubk\u00E1ch 0,05 - 0,1 m a 0,25 - 0,3m srovnateln\u00E9 u obou variant, v hloubce 0,15 - 0,2 m byly vy\u0161\u0161\u00ED u CT. Obsahy humusov\u00FDch l\u00E1tek (Cox HL ? ? HK+FK) a horkovodorozpustn\u00E9ho uhl\u00EDku (Chws) byly p\u0159ibli\u017En\u011B stejn\u00E9 u obou variant zpracov\u00E1n\u00ED ve v\u0161ech" . "121-127" . . . "80-7040-818-9" . "Changes of soil properties under minimum tillage in different soil-climatic conditions"@en . . "[8FD79EBEDF92]" . . "Nov\u00E9 Hrady" . . "Zm\u011Bny vlastnost\u00ED p\u016Fdy p\u0159i bezorebn\u00E9m zpracov\u00E1n\u00ED v rozd\u00EDln\u00FDch p\u016Fdn\u011B -klimatick\u00FDch podm\u00EDnk\u00E1ch" . "V p\u0159esn\u00E9m velkoparcelkov\u00E9m (\u010Dernozem - Gross Enzerdorf) a st\u0159edn\u011Bdob\u00E9m provozn\u00EDm (kambizem - Stagra Studen\u00E1) pokusu jsou sledov\u00E1ny vybran\u00E9 fyzik\u00E1ln\u011B chemick\u00E9 vlastnosti p\u016Fdy p\u0159i porovn\u00E1n\u00ED bezorebn\u00E9 (MT( a konven\u010Dn\u00ED (CT) technologie technologie jej\u00EDho zpracov\u00E1n\u00ED v p\u016Fdn\u00EDm profilu na ja\u0159e a na podzim. Fyzik\u00E1ln\u00ED parametry p\u016Fdy byly u kambizem\u011B p\u0159\u00EDzniv\u011Bj\u0161\u00ED u CT v hloubce 0,2 m, v hloubce 0,25 - 0,30 m byly ji\u017E hodnoty srovnateln\u00E9 nebo m\u00EDrn\u011B p\u0159\u00EDzniv\u011Bj\u0161\u00ED u MT. U \u010Dernozem\u011B byly naopak vlhkostn\u00ED pom\u011Bry v pr\u016Fb\u011Bhuroku lep\u0161\u00ED u MT v cel\u00E9m p\u016Fdn\u00EDm profilu. Or zde byla do hloubky 0,3 m u MT rovnom\u011Brn\u011Bj\u0161\u00ED ,ale nepatrn\u011B vy\u0161\u0161\u00ED ne\u017E v CT a do hloubky 0,5 m se sni\u017Euje. U CT doch\u00E1z\u00ED v hloubce 0,3 - 0,4 m naopak k jej\u00EDmu zv\u00FD\u0161en\u00ED. Pr\u016Fm\u011Brn\u00E9 obsahy celkov\u00E9ho uhl\u00EDku (Cox) byly ukambizem\u011B v hloubk\u00E1ch 0,05 - 0,1 m a 0,25 - 0,3m srovnateln\u00E9 u obou variant, v hloubce 0,15 - 0,2 m byly vy\u0161\u0161\u00ED u CT. Obsahy humusov\u00FDch l\u00E1tek (Cox HL ? ? HK+FK) a horkovodorozpustn\u00E9ho uhl\u00EDku (Chws) byly p\u0159ibli\u017En\u011B stejn\u00E9 u obou variant zpracov\u00E1n\u00ED ve v\u0161ech"@cs . "RIV/60076658:12220/05:00006247" .