"P(1G57016)" . "1"^^ . . . "Stanoven\u00ED nebezpe\u010D\u00ED povrchov\u00E9ho odtoku a n\u00E1sledn\u00E9 eroze ve smrkov\u00FDch porostech na prudk\u00FDch svaz\u00EDch p\u0159i r\u016Fzn\u00FDch zp\u016Fsobech obnovy (hol\u00E1 se\u010D, clonn\u00E1 se\u010D, mate\u0159sk\u00FD porost)"@cs . "Stanoven\u00ED nebezpe\u010D\u00ED povrchov\u00E9ho odtoku a n\u00E1sledn\u00E9 eroze ve smrkov\u00FDch porostech na prudk\u00FDch svaz\u00EDch p\u0159i r\u016Fzn\u00FDch zp\u016Fsobech obnovy (hol\u00E1 se\u010D, clonn\u00E1 se\u010D, mate\u0159sk\u00FD porost)" . . . "Assessment of overland flow and following erosion hazard in Norway spruce stands on steep slopes using different regeneration methods (clearcutting, shelterwood cutting, and mature stand)"@en . . . "forest regeneration; Norway spruce stand; steep south-facing slope; silvicultural methods; clearcutting; shelterwood cutting; precipitation; hillslope runoff; overland flow; soil erosion hazard"@en . . "452119" . "Assessment of overland flow and following erosion hazard in Norway spruce stands on steep slopes using different regeneration methods (clearcutting, shelterwood cutting, and mature stand)"@en . . "\u0160ach, Franti\u0161ek" . . . . "RIV/00020702:_____/07:8P008246" . . . "Vyhodnocen\u00ED 29let\u00E9 \u0159ady pozorov\u00E1n\u00ED na stacion\u00E1ru \u010Cesk\u00E1 \u010Cermn\u00E1, posouzen\u00ED a kvantifikace svahov\u00E9ho odtoku (zejm\u00E9na jeho povrchov\u00E9 formy) umo\u017Enily hodnotit tak\u00E9 mo\u017En\u00E9 erozivn\u00ED n\u00E1sledky na hol\u00E9 se\u010Di (H) i clonn\u00E9 se\u010Di (C) a v kontroln\u00ED smrkov\u00E9 kmenovin\u011B (K) na prudk\u00E9m ji\u017En\u00EDm svahu (sklon 21\u00B0, 5K1, 5N1, 460 \u2013 540 m n.m.) p\u0159i rozd\u00EDln\u00E9 velikosti a intenzit\u011B sr\u00E1\u017Eek. Obnovn\u00ED postupy holose\u010Dn\u00FD ani clonose\u010Dn\u00FD nevyvolaly na t\u011B\u017Een\u00FDch ploch\u00E1ch povrchov\u00FD odtok s n\u00E1slednou vodn\u00ED eroz\u00ED p\u016Fdy. Ani samotn\u00E1 hol\u00E1 se\u010D neporu\u0161en\u00E1 pojezdem mechaniza\u010Dn\u00EDch prost\u0159edk\u016F tedy nem\u011Bla za n\u00E1sledek povrchov\u00FD odtok doprov\u00E1zen\u00FD \u201Eon-site\u201C vodn\u00ED eroz\u00ED p\u016Fdy. Nenastaly ani p\u0159i vysok\u00FDch a intenzivn\u00EDch de\u0161\u0165ov\u00FDch sr\u00E1\u017Ek\u00E1ch ve vegeta\u010Dn\u00EDm obdob\u00ED, kdy jsou nejfrekventovan\u011Bj\u0161\u00ED. Obnovn\u00ED postupy v\u0161ak mohou ovliv\u0148ovat svahov\u00FD odtok s n\u00E1slednou \u201Eoff-site\u201C vodn\u00ED eroz\u00ED zejm\u00E9na ze zp\u0159\u00EDstup\u0148ovac\u00ED s\u00EDt\u011B (a objekt\u016F) a z hydrografick\u00E9 s\u00EDt\u011B (a objekt\u016F). Pro ur\u010Den\u00ED rizika off-site eroze byl navr\u017Een praktick\u00FD postup stanoven\u00ED erozivn\u011B rizikov\u00E9ho svahov\u00E9ho odtoku." . . . "[882CFABDAA52]" . . . . . . "RIV/00020702:_____/07:8P008246!RIV08-MZE-00020702" . "Vyhodnocen\u00ED 29let\u00E9 \u0159ady pozorov\u00E1n\u00ED na stacion\u00E1ru \u010Cesk\u00E1 \u010Cermn\u00E1, posouzen\u00ED a kvantifikace svahov\u00E9ho odtoku (zejm\u00E9na jeho povrchov\u00E9 formy) umo\u017Enily hodnotit tak\u00E9 mo\u017En\u00E9 erozivn\u00ED n\u00E1sledky na hol\u00E9 se\u010Di (H) i clonn\u00E9 se\u010Di (C) a v kontroln\u00ED smrkov\u00E9 kmenovin\u011B (K) na prudk\u00E9m ji\u017En\u00EDm svahu (sklon 21\u00B0, 5K1, 5N1, 460 \u2013 540 m n.m.) p\u0159i rozd\u00EDln\u00E9 velikosti a intenzit\u011B sr\u00E1\u017Eek. Obnovn\u00ED postupy holose\u010Dn\u00FD ani clonose\u010Dn\u00FD nevyvolaly na t\u011B\u017Een\u00FDch ploch\u00E1ch povrchov\u00FD odtok s n\u00E1slednou vodn\u00ED eroz\u00ED p\u016Fdy. Ani samotn\u00E1 hol\u00E1 se\u010D neporu\u0161en\u00E1 pojezdem mechaniza\u010Dn\u00EDch prost\u0159edk\u016F tedy nem\u011Bla za n\u00E1sledek povrchov\u00FD odtok doprov\u00E1zen\u00FD \u201Eon-site\u201C vodn\u00ED eroz\u00ED p\u016Fdy. Nenastaly ani p\u0159i vysok\u00FDch a intenzivn\u00EDch de\u0161\u0165ov\u00FDch sr\u00E1\u017Ek\u00E1ch ve vegeta\u010Dn\u00EDm obdob\u00ED, kdy jsou nejfrekventovan\u011Bj\u0161\u00ED. Obnovn\u00ED postupy v\u0161ak mohou ovliv\u0148ovat svahov\u00FD odtok s n\u00E1slednou \u201Eoff-site\u201C vodn\u00ED eroz\u00ED zejm\u00E9na ze zp\u0159\u00EDstup\u0148ovac\u00ED s\u00EDt\u011B (a objekt\u016F) a z hydrografick\u00E9 s\u00EDt\u011B (a objekt\u016F). Pro ur\u010Den\u00ED rizika off-site eroze byl navr\u017Een praktick\u00FD postup stanoven\u00ED erozivn\u011B rizikov\u00E9ho svahov\u00E9ho odtoku."@cs . "Stanoven\u00ED nebezpe\u010D\u00ED povrchov\u00E9ho odtoku a n\u00E1sledn\u00E9 eroze ve smrkov\u00FDch porostech na prudk\u00FDch svaz\u00EDch p\u0159i r\u016Fzn\u00FDch zp\u016Fsobech obnovy (hol\u00E1 se\u010D, clonn\u00E1 se\u010D, mate\u0159sk\u00FD porost)" . . "Assessment of 29 year series of observations on the long term research area \u010Cesk\u00E1 \u010Cermn\u00E1, judgment and quantification of hillslope runoff (overland flow in particular) enabled to evaluate also possible erosive effects on the clear cut plot (H), shelterwood harvested plot, and mature Norway spruce stand plot (K) on steep south-facing slope (inclination of 21 degree, altitude of 460-540 m, stony acid fir-beechwood site type) at different precipitation depth and intensity. Neither the clearcut method nor the shelterwood method caused on harvested plots overland flow and consequent soil erosion. The clearcutting itself, without disturbances by high lead yarding or skidding, did not trigger overland flow accompanied by \u201Eon-site\u201C soil erosion. They did not arise either at rainstorms or at long-lasting heavy rainfalls during growing period when they are most frequent. Regeneration methods would influence hillslope runoff with consequent \u201Eoff-site\u201C soil erosion from the forest road access and drainage network"@en . "Stanoven\u00ED nebezpe\u010D\u00ED povrchov\u00E9ho odtoku a n\u00E1sledn\u00E9 eroze ve smrkov\u00FDch porostech na prudk\u00FDch svaz\u00EDch p\u0159i r\u016Fzn\u00FDch zp\u016Fsobech obnovy (hol\u00E1 se\u010D, clonn\u00E1 se\u010D, mate\u0159sk\u00FD porost)"@cs . "1"^^ . .