"527581" . "525;531" . . . "Kvantifikace re\u017Eimu podzemn\u00EDch vod p\u0159i extr\u00E9mn\u00EDch hydrologick\u00FDch situac\u00EDch" . "RIV/00020711:_____/05:00000771" . . "Kvantifikace re\u017Eimu podzemn\u00EDch vod p\u0159i extr\u00E9mn\u00EDch hydrologick\u00FDch situac\u00EDch"@cs . "2"^^ . . "Kvantifikace re\u017Eimu podzemn\u00EDch vod p\u0159i extr\u00E9mn\u00EDch hydrologick\u00FDch situac\u00EDch" . . "7"^^ . "Proper management of groundwater resources depends on the knowledge how to calculate changes in groundwater quantity. Determination of the volume of active groundwater storage (storage above pertinent erosive base) is shown by examples of two different basins. The first type is a structure with deep circulation and huge accumulation (the Police Cretaceous basin), the second type is a structure with shallow circulation (the Eagle Mountains crystalline complex). Reduction of groundwater storage in decrease periods was computed by the SIMBA hydrological balance model. This study shows that deficits of the active storage in the basin structure are for the time being acceptable, but in the crystalline structure the active storage is often almost completely exhausted. Relation between change of groundwater storage and change of groundwater level in the Police basin was deduced, followed by another relation between change of groundwater storage and change of spring yield in the Eagle Mountains crystalline co"@en . . "Pro mo\u017Enost hospoda\u0159en\u00ED s podzemn\u00EDmi vodami a stanoven\u00ED jejich vodohospod\u00E1\u0159sk\u00E9ho v\u00FDznamu je nezbytn\u00E9 kvantifikovat jejich re\u017Eim. Na p\u0159\u00EDkladech dvou vodom\u011Brn\u00FDch profil\u016F Metuje, Teplice n. M. (89 km2) a Hronov (240 km2) v k\u0159\u00EDdov\u00E9 Polick\u00E9 p\u00E1nvi (struktura shlubok\u00FDm ob\u011Bhem a velkou akumulac\u00ED) a profilu Divok\u00E9 Orlice, Kl\u00E1\u0161terec n. O. (155 km2) v krystaliniku Orlick\u00FDch hor (struktura s m\u011Blk\u00FDm ob\u011Bhem podzemn\u00ED vody) jsme stanovili velikosti aktivn\u00EDch z\u00E1sob podzemn\u00ED vody (objem podzemn\u00ED vody nad \u00FArovn\u00ED p\u0159\u00EDslu\u0161n \u00E9 erozn\u00ED z\u00E1kladny). Podle modelu hydrologick\u00E9 bilance byly ur\u010Deny velikosti jejich zmen\u0161ov\u00E1n\u00ED v obdob\u00EDch poklesu, kdy je odtok z povod\u00ED tvo\u0159en v\u00FDlu\u010Dn\u011B dotac\u00ED podzemn\u00EDch vod. Uk\u00E1zalo se, \u017Ee deficity aktivn\u00ED z\u00E1soby jsou v p\u00E1nevn\u00ED struktu\u0159e za sou\u010Dasn\u00FDch podm\u00EDnek p\u0159ijateln\u00E9 i v extr\u00E9mn\u00EDch p\u0159\u00EDpadech, v krystaliniku horsk\u00E9 oblasti v\u0161ak doch\u00E1z\u00ED a\u017E k jej\u00EDmu \u00FApln\u00E9mu vy\u010Derp\u00E1n\u00ED. Je odvozen vztah zm\u011Bn z\u00E1sob ke zm\u011Bn\u00E1m hladiny podzemn\u00ED vody v Polick\u00E9 p\u00E1nvi, respektive ke zm\u011Bn\u011B vydatnosti pramen\u016F v oblasti krystalini" . "80-88907-53-5" . . . "[A4679BB7DF91]" . . . . "RIV/00020711:_____/05:00000771!RIV06-MZP-00020711" . "Ministerstvo \u017Eivotn\u00EDho prost\u0159ed\u00ED \u010CR" . . . . "Kr\u00E1tk\u00E1, Martina" . . . "2005-09-21+02:00"^^ . . "Pro mo\u017Enost hospoda\u0159en\u00ED s podzemn\u00EDmi vodami a stanoven\u00ED jejich vodohospod\u00E1\u0159sk\u00E9ho v\u00FDznamu je nezbytn\u00E9 kvantifikovat jejich re\u017Eim. Na p\u0159\u00EDkladech dvou vodom\u011Brn\u00FDch profil\u016F Metuje, Teplice n. M. (89 km2) a Hronov (240 km2) v k\u0159\u00EDdov\u00E9 Polick\u00E9 p\u00E1nvi (struktura shlubok\u00FDm ob\u011Bhem a velkou akumulac\u00ED) a profilu Divok\u00E9 Orlice, Kl\u00E1\u0161terec n. O. (155 km2) v krystaliniku Orlick\u00FDch hor (struktura s m\u011Blk\u00FDm ob\u011Bhem podzemn\u00ED vody) jsme stanovili velikosti aktivn\u00EDch z\u00E1sob podzemn\u00ED vody (objem podzemn\u00ED vody nad \u00FArovn\u00ED p\u0159\u00EDslu\u0161n \u00E9 erozn\u00ED z\u00E1kladny). Podle modelu hydrologick\u00E9 bilance byly ur\u010Deny velikosti jejich zmen\u0161ov\u00E1n\u00ED v obdob\u00EDch poklesu, kdy je odtok z povod\u00ED tvo\u0159en v\u00FDlu\u010Dn\u011B dotac\u00ED podzemn\u00EDch vod. Uk\u00E1zalo se, \u017Ee deficity aktivn\u00ED z\u00E1soby jsou v p\u00E1nevn\u00ED struktu\u0159e za sou\u010Dasn\u00FDch podm\u00EDnek p\u0159ijateln\u00E9 i v extr\u00E9mn\u00EDch p\u0159\u00EDpadech, v krystaliniku horsk\u00E9 oblasti v\u0161ak doch\u00E1z\u00ED a\u017E k jej\u00EDmu \u00FApln\u00E9mu vy\u010Derp\u00E1n\u00ED. Je odvozen vztah zm\u011Bn z\u00E1sob ke zm\u011Bn\u00E1m hladiny podzemn\u00ED vody v Polick\u00E9 p\u00E1nvi, respektive ke zm\u011Bn\u011B vydatnosti pramen\u016F v oblasti krystalini"@cs . "Bratislava" . "Bratislava" . . "Kn\u011B\u017Eek, Miroslav" . . "Hydrologick\u00E9 dni 2005" . . "Z(MZP0002071101)" . "baseflow; groundwater storage; hydrological balance; borehole; spring, the Police basin; the Eagle Mountains"@en . "Kvantifikace re\u017Eimu podzemn\u00EDch vod p\u0159i extr\u00E9mn\u00EDch hydrologick\u00FDch situac\u00EDch"@cs . "3"^^ . "Quantification of groundwater regime during extreme hydrological situations"@en . "Quantification of groundwater regime during extreme hydrological situations"@en .