. "2013-05-22+02:00"^^ . "Du\u0161ek, Radek" . . "100548" . "17310" . . "Protierozn\u00ED opat\u0159en\u00ED tzv. lok\u00E1ln\u00EDho roz\u0161\u00ED\u0159en\u00ED koryta na \u0159ece Mor\u00E1vce - idea, funkce a monitoring (Moravskoslezsk\u00E9 Beskydy, \u010Cesk\u00E1 republika)"@cs . . . "\u0160karpich, V\u00E1clav" . "B\u011Bhem posledn\u00EDch sto let bylo koryto \u0159eky Mor\u00E1vky v p\u0159edpol\u00ED Moravskoslezsk\u00FDch Beskyd transformov\u00E1no z v\u011Btv\u00EDc\u00EDho se \u0159\u00ED\u010Dn\u00EDho vzoru v jednoduch\u00E9 koryto se zachoval\u00FDm \u0161t\u011Brkonosn\u00FDm charakterem. Na mnoha m\u00EDstech do\u0161lo tak\u00E9 k v\u00FDrazn\u00E9mu zahlouben\u00ED do skaln\u00EDho podlo\u017E\u00ED. Tato transformace byla ve velk\u00E9 m\u00ED\u0159e predisponov\u00E1na antropogenn\u00EDm tlakem ve form\u011B zm\u011Bn vyu\u017Eit\u00ED krajiny a krajinn\u00E9ho krytu, regulac\u00ED koryt a v\u00FDstavbou bari\u00E9r na toku (jezy, \u00FAdoln\u00ED n\u00E1dr\u017Ee). Vyj\u00EDme\u010Dn\u00FD z hlediska zachov\u00E1n\u00ED p\u016Fvodn\u00EDho v\u011Btv\u00EDc\u00EDho se \u0159\u00ED\u010Dn\u00EDho vzoru \u0161t\u011Brkonosn\u00E9ho charakteru je \u00FAsek \u0159eky Mor\u00E1vky na \u0159. km 7,0 a\u017E 10,5." . . . "RIV/61988987:17310/13:A14017QR" . . . "accelerated deep erosion; (dis)connectivity of the sediment movement; Mor\u00E1vka River; Moravskoslezsk\u00E9 Beskydy Mts; Czech Republic."@en . . "Protierozn\u00ED opat\u0159en\u00ED tzv. lok\u00E1ln\u00EDho roz\u0161\u00ED\u0159en\u00ED koryta na \u0159ece Mor\u00E1vce - idea, funkce a monitoring (Moravskoslezsk\u00E9 Beskydy, \u010Cesk\u00E1 republika)"@cs . "B\u011Bhem posledn\u00EDch sto let bylo koryto \u0159eky Mor\u00E1vky v p\u0159edpol\u00ED Moravskoslezsk\u00FDch Beskyd transformov\u00E1no z v\u011Btv\u00EDc\u00EDho se \u0159\u00ED\u010Dn\u00EDho vzoru v jednoduch\u00E9 koryto se zachoval\u00FDm \u0161t\u011Brkonosn\u00FDm charakterem. Na mnoha m\u00EDstech do\u0161lo tak\u00E9 k v\u00FDrazn\u00E9mu zahlouben\u00ED do skaln\u00EDho podlo\u017E\u00ED. Tato transformace byla ve velk\u00E9 m\u00ED\u0159e predisponov\u00E1na antropogenn\u00EDm tlakem ve form\u011B zm\u011Bn vyu\u017Eit\u00ED krajiny a krajinn\u00E9ho krytu, regulac\u00ED koryt a v\u00FDstavbou bari\u00E9r na toku (jezy, \u00FAdoln\u00ED n\u00E1dr\u017Ee). Vyj\u00EDme\u010Dn\u00FD z hlediska zachov\u00E1n\u00ED p\u016Fvodn\u00EDho v\u011Btv\u00EDc\u00EDho se \u0159\u00ED\u010Dn\u00EDho vzoru \u0161t\u011Brkonosn\u00E9ho charakteru je \u00FAsek \u0159eky Mor\u00E1vky na \u0159. km 7,0 a\u017E 10,5."@cs . . "Protierozn\u00ED opat\u0159en\u00ED tzv. lok\u00E1ln\u00EDho roz\u0161\u00ED\u0159en\u00ED koryta na \u0159ece Mor\u00E1vce - idea, funkce a monitoring (Moravskoslezsk\u00E9 Beskydy, \u010Cesk\u00E1 republika)" . . "P(GP205/06/P131)" . . "Protierozn\u00ED opat\u0159en\u00ED tzv. lok\u00E1ln\u00EDho roz\u0161\u00ED\u0159en\u00ED koryta na \u0159ece Mor\u00E1vce - idea, funkce a monitoring (Moravskoslezsk\u00E9 Beskydy, \u010Cesk\u00E1 republika)" . "6"^^ . . "Anti-erosive measures in the Mor\u00E1vka River - Sense, Function And Monitoring (Moravskoslezsk\u00E9 Beskydy Mts, Czech Republic)"@en . . "Zborn\u00EDk predn\u00E1\u0161ok zo VII. konferencie s medzin\u00E1rodnou \u00FA\u010Das\u0165ou - Sedimenty vodn\u00FDch tokov a n\u00E1dr\u017E\u00ED" . . "Galia, Tom\u00E1\u0161" . . "Bratislava" . "Anti-erosive measures in the Mor\u00E1vka River - Sense, Function And Monitoring (Moravskoslezsk\u00E9 Beskydy Mts, Czech Republic)"@en . "Hradeck\u00FD, Jan" . "978-80-89062-90-4" . "Bratislava" . "[5F519EAD3F1A]" . "4"^^ . . "During the last century the Mor\u00E1vka River channel has been transformed from anabranching to single channel river pattern that incised as deep as the bedrock. These changes have been caused by a strong man impact in the form of the land use and land cover changes, river channel controlling, bank stabilising, weir and valley dam constructing. Contemporary channel changes have not been evident at reach r. km 7.0 to 10.5 which has partly preserved the original anabranching river pattern with lateral erosion a sediment movement. In order to preserve this anabranching river reach and the prevention of proceeding backward erosion and potential Vy\u0161n\u00ED Lhoty weir destruction at r. km 11.3 were constructed anti-erosion dykes (at r. km 10.7)."@en . . . "4"^^ . "RIV/61988987:17310/13:A14017QR!RIV14-GA0-17310___" . . . "Slovensk\u00E1 vodohospod\u00E1rska spolo\u010Dnos\u0165" .