"\u010Cesk\u00E1 asociace hydrogeolog\u016F" . "P(AACBU31-03)" . "4"^^ . "Posouzen\u00ED mo\u017Enost\u00ED zp\u011Btn\u00E9ho p\u0159estupu vod do uzav\u0159en\u00E9ho vodn\u00EDho t\u011Blesa ?detritu? v OKR. P\u0159estup vod se m\u016F\u017Ee realizovat jedin\u011B plochami, kter\u00E9 vznikly antropogenn\u011B hornickou \u010Dinnost\u00ED. P\u0159estupn\u00ED plochy ? resp. koeficient hydraulick\u00E9 vodivosti se v\u0161ak ve velmi kr\u00E1tk\u00E9m \u010Dase zm\u011Bn\u00ED. Pro zp\u011Btn\u00FD p\u0159etok d\u016Fln\u00EDch vod do detritu mus\u00ED existovat nyn\u00ED tak vysok\u00FD hydraulick\u00FD sp\u00E1d, kter\u00FD p\u0159ekon\u00E1 v\u0161echny odpory st\u00E1vaj\u00EDc\u00EDho zvodn\u011Bn\u00E9ho syst\u00E9mu. Znamen\u00E1 to, \u017Ee hydraulick\u00FD sp\u00E1d mus\u00ED dos\u00E1hnout nejen p\u016Fvodn\u00EDho stavu p\u016Fvodn\u00EDho hydraulick\u00E9ho re\u017Eimu, ale mus\u00ED b\u00FDt vy\u0161\u0161\u00ED. P\u0159edpokl\u00E1d\u00E1me, \u017Ee p\u0159etok z detritu bude natolik minimalizov\u00E1n, \u017Ee nebude posti\u017Eiteln\u00FD v re\u00E1ln\u00E9m \u010Dase v m\u011B\u0159iteln\u00FDch hodnot\u00E1ch."@cs . . . "RIV/61989100:_____/09:00022233!RIV10-CBU-61989100" . "Jel\u00EDnek, Petr" . "RIV/61989100:_____/09:00022233" . . "Posouzen\u00ED mo\u017Enost\u00ED zp\u011Btn\u00E9ho p\u0159estupu vod do uzav\u0159en\u00E9ho vodn\u00EDho t\u011Blesa ?detritu? v OKR. P\u0159estup vod se m\u016F\u017Ee realizovat jedin\u011B plochami, kter\u00E9 vznikly antropogenn\u011B hornickou \u010Dinnost\u00ED. P\u0159estupn\u00ED plochy ? resp. koeficient hydraulick\u00E9 vodivosti se v\u0161ak ve velmi kr\u00E1tk\u00E9m \u010Dase zm\u011Bn\u00ED. Pro zp\u011Btn\u00FD p\u0159etok d\u016Fln\u00EDch vod do detritu mus\u00ED existovat nyn\u00ED tak vysok\u00FD hydraulick\u00FD sp\u00E1d, kter\u00FD p\u0159ekon\u00E1 v\u0161echny odpory st\u00E1vaj\u00EDc\u00EDho zvodn\u011Bn\u00E9ho syst\u00E9mu. Znamen\u00E1 to, \u017Ee hydraulick\u00FD sp\u00E1d mus\u00ED dos\u00E1hnout nejen p\u016Fvodn\u00EDho stavu p\u016Fvodn\u00EDho hydraulick\u00E9ho re\u017Eimu, ale mus\u00ED b\u00FDt vy\u0161\u0161\u00ED. P\u0159edpokl\u00E1d\u00E1me, \u017Ee p\u0159etok z detritu bude natolik minimalizov\u00E1n, \u017Ee nebude posti\u017Eiteln\u00FD v re\u00E1ln\u00E9m \u010Dase v m\u011B\u0159iteln\u00FDch hodnot\u00E1ch." . . . "fossil water; Lower Badenian basal clastics; Upper Silesian Basin; back water transfer"@en . . . "Projevy antropogenn\u00EDho naru\u0161en\u00ED hydraulick\u00E9 izolace a mo\u017Enost zp\u011Btn\u00E9ho p\u0159estupu d\u016Fln\u00EDch vod do zvodn\u011Bn\u00E9ho syst\u00E9mu baz\u00E1ln\u00EDch klastik sp. badenu v OKR" . . "Grmela, Arno\u0161t" . "Projevy antropogenn\u00EDho naru\u0161en\u00ED hydraulick\u00E9 izolace a mo\u017Enost zp\u011Btn\u00E9ho p\u0159estupu d\u016Fln\u00EDch vod do zvodn\u011Bn\u00E9ho syst\u00E9mu baz\u00E1ln\u00EDch klastik sp. badenu v OKR"@cs . . . "3"^^ . "2009-08-31+02:00"^^ . . "Projevy antropogenn\u00EDho naru\u0161en\u00ED hydraulick\u00E9 izolace a mo\u017Enost zp\u011Btn\u00E9ho p\u0159estupu d\u016Fln\u00EDch vod do zvodn\u011Bn\u00E9ho syst\u00E9mu baz\u00E1ln\u00EDch klastik sp. badenu v OKR"@cs . "978-80-248-2026-2" . "Ostrava" . "1"^^ . "Ostrava" . . "337079" . . . "[06CAA1F90A9E]" . "Projevy antropogenn\u00EDho naru\u0161en\u00ED hydraulick\u00E9 izolace a mo\u017Enost zp\u011Btn\u00E9ho p\u0159estupu d\u016Fln\u00EDch vod do zvodn\u011Bn\u00E9ho syst\u00E9mu baz\u00E1ln\u00EDch klastik sp. badenu v OKR" . "Dvorsk\u00FD, Ji\u0159\u00ED" . "Effect of Anthropogenic Damage to Hydraulic Isolation and Possibilities of Transfer of Mine Water Back to the Water-Bearing System of Lower Badenian Basal Clastics in the Ostrava-Karvin\u00E1 Coalfield"@en . . . . "The evaluation of possibilities of transfer of water back to the closed water body of ?detritus? in the Ostrava-Karvin\u00E1 Coalfield is presented. Water transfer can occur only through those planes that have been formed anthropogenically by mining activity. However, the transfer planes ? or the hydraulic conductivity coefficient will change in a very short time. For the flow of mine water back to the detritus, the sufficient hydraulic gradient that is able to overcome the resistance of the existing water-bearing system must exist. This means that the hydraulic gradient must not only achieve the initial state of initial hydraulic regime; it must be even higher. We expect that the transfer from detritus will be so minimized that it will not be measurable in real time."@en . "10. \u010Desko-slovensk\u00FD mezin\u00E1rodn\u00ED hydrogeologick\u00FD kongres" . "Effect of Anthropogenic Damage to Hydraulic Isolation and Possibilities of Transfer of Mine Water Back to the Water-Bearing System of Lower Badenian Basal Clastics in the Ostrava-Karvin\u00E1 Coalfield"@en .