"1"^^ . . "Olomouc" . "Vliv vybran\u00FDch \u010Dinitel\u016F na dynamiku p\u016Fdn\u00ED vlhkosti n\u00ED\u017Einn\u00E9ho \u00FAzem\u00ED" . "Olomouc" . . "2009-01-01+01:00"^^ . "43210" . . "Effect of selected factors on the dynamics of soil moisture in lowland"@en . . "Vliv vybran\u00FDch \u010Dinitel\u016F na dynamiku p\u016Fdn\u00ED vlhkosti n\u00ED\u017Einn\u00E9ho \u00FAzem\u00ED"@cs . . "349670" . "[86CD5F993C5A]" . "Vl\u010Dek, V\u00EDt\u011Bzslav" . "Vliv vybran\u00FDch \u010Dinitel\u016F na dynamiku p\u016Fdn\u00ED vlhkosti n\u00ED\u017Einn\u00E9ho \u00FAzem\u00ED" . . "The present work assesses the impact of three selected hydro-meteorological parameters for the years 2005-2007 (the water level in an underground borehole, the level of water in the river Svratka and rainfall) on soil moisture at a depth of 70 cm. Soils on the site is gleyic fluvisol (FLq). Tested area is located on the experimental field of Mendel University of Agriculture and Forestry in Brno in the \u017Dab\u010Dice village (20 km south of Brno). The annual temperature is 9.2\u00B0 C, annual rain normal 483 mm. The most appeared to influence the level of groundwater in the borehole (55.25% of variance of moisture at a depth of 70 cm, is related to the height of groundwater level in borehole Nosislav), 33.66% moisture dissipation, related to the level of water in the Svratka river, 3.22% of variance of moisture at a depth of 70 cm, is related to precipitation, the remaining 7.87% goes to other factors not included here."@en . . "RIV/62156489:43210/09:00144770!RIV10-MSM-43210___" . "RIV/62156489:43210/09:00144770" . "P(2B06101)" . "\u0158\u00ED\u010Dn\u00ED krajina 6. Sborn\u00EDk p\u0159\u00EDsp\u011Bvk\u016F z konference." . . "Effect of selected factors on the dynamics of soil moisture in lowland"@en . "6"^^ . . . "soil moisture; river landscape"@en . . . . "Pr\u00E1ce hodnot\u00ED vliv t\u0159\u00ED vybran\u00FDch hydrometeorologick\u00FDch parametr\u016F (hladiny podzemn\u00ED vody ve vrtu, hladiny vody v \u0159ece Svratce a sr\u00E1\u017Ekov\u00FDch \u00FAhrn\u016F) na vlhkost p\u016Fdy v hloubce 70 cm v letech 2005 -- 2007. M\u011B\u0159en\u00ED vlhkost\u00ED p\u016Fdy prob\u00EDhala na pokusn\u00E9m pozemku v \u017Dab\u010Dic\u00EDch u Brna v kuku\u0159i\u010Dn\u00E9 v\u00FDrobn\u00ED oblasti na t\u011B\u017Ek\u00E9 p\u016Fd\u011B (fluvizem glejov\u00E1) s porostem kuku\u0159ice. Nejv\u00FDznamn\u011Bj\u0161\u00ED vliv na vlhkost p\u016Fdy m\u011Bly stavy podzemn\u00ED vody ve vrtu (55,25 % rozptylu vlhkosti v hloubce 70 cm). 33,66 % rozptyl\u016F vlhkosti p\u016Fdy v hloubce 70 cm bylo ovlivn\u011Bno stavy \u0159eky Svratky a jen 7,87 % sr\u00E1\u017Ekami. V\u00FDrazn\u00FDm vlivem, kter\u00FD p\u016Fsob\u00ED na vztah p\u016Fdn\u00ED vlhkosti s hladinou podzemn\u00ED vody, hladinou Svratky nebo sr\u00E1\u017Ekov\u00FDmi \u00FAhrny, je evapotranspirace porostu kuku\u0159ice. Rostlina kuku\u0159ice spot\u0159ebov\u00E1v\u00E1 k produkci vysok\u00E9ho mno\u017Estv\u00ED biomasy velk\u00E9 mno\u017Estv\u00ED vody a ovliv\u0148uje tak v\u00FDrazn\u011B vlhkost p\u016Fdy v pom\u011Brn\u011B velk\u00E9 hloubce (a\u017E 1,5 m). Anal\u00FDzy uk\u00E1zaly velmi v\u00FDraznou vazbu mezi hydrick\u00FDm re\u017Eimem \u0159eky Svratky a vlhkost\u00ED p\u016Fdy v zem\u011Bd\u011Blsky vyu\u017E\u00EDvan\u00E9 krajin\u011B." . . "St\u0159eda, Tom\u00E1\u0161" . "978-80-244-2358-6" . "Vliv vybran\u00FDch \u010Dinitel\u016F na dynamiku p\u016Fdn\u00ED vlhkosti n\u00ED\u017Einn\u00E9ho \u00FAzem\u00ED"@cs . "UPOL, \u010Cesk\u00E1 spole\u010Dnost pro krajinnou ekologii" . . "Pr\u00E1ce hodnot\u00ED vliv t\u0159\u00ED vybran\u00FDch hydrometeorologick\u00FDch parametr\u016F (hladiny podzemn\u00ED vody ve vrtu, hladiny vody v \u0159ece Svratce a sr\u00E1\u017Ekov\u00FDch \u00FAhrn\u016F) na vlhkost p\u016Fdy v hloubce 70 cm v letech 2005 -- 2007. M\u011B\u0159en\u00ED vlhkost\u00ED p\u016Fdy prob\u00EDhala na pokusn\u00E9m pozemku v \u017Dab\u010Dic\u00EDch u Brna v kuku\u0159i\u010Dn\u00E9 v\u00FDrobn\u00ED oblasti na t\u011B\u017Ek\u00E9 p\u016Fd\u011B (fluvizem glejov\u00E1) s porostem kuku\u0159ice. Nejv\u00FDznamn\u011Bj\u0161\u00ED vliv na vlhkost p\u016Fdy m\u011Bly stavy podzemn\u00ED vody ve vrtu (55,25 % rozptylu vlhkosti v hloubce 70 cm). 33,66 % rozptyl\u016F vlhkosti p\u016Fdy v hloubce 70 cm bylo ovlivn\u011Bno stavy \u0159eky Svratky a jen 7,87 % sr\u00E1\u017Ekami. V\u00FDrazn\u00FDm vlivem, kter\u00FD p\u016Fsob\u00ED na vztah p\u016Fdn\u00ED vlhkosti s hladinou podzemn\u00ED vody, hladinou Svratky nebo sr\u00E1\u017Ekov\u00FDmi \u00FAhrny, je evapotranspirace porostu kuku\u0159ice. Rostlina kuku\u0159ice spot\u0159ebov\u00E1v\u00E1 k produkci vysok\u00E9ho mno\u017Estv\u00ED biomasy velk\u00E9 mno\u017Estv\u00ED vody a ovliv\u0148uje tak v\u00FDrazn\u011B vlhkost p\u016Fdy v pom\u011Brn\u011B velk\u00E9 hloubce (a\u017E 1,5 m). Anal\u00FDzy uk\u00E1zaly velmi v\u00FDraznou vazbu mezi hydrick\u00FDm re\u017Eimem \u0159eky Svratky a vlhkost\u00ED p\u016Fdy v zem\u011Bd\u011Blsky vyu\u017E\u00EDvan\u00E9 krajin\u011B."@cs . "2"^^ .