. . "Nestabilitou hnan\u00E9 proud\u011Bn\u00ED a tvorba odtoku v mal\u00E9m povod\u00ED"@cs . . . "Nestabilitou hnan\u00E9 proud\u011Bn\u00ED a tvorba odtoku v mal\u00E9m povod\u00ED"@cs . . . "rainfall; runoff; soil"@en . "1695-6133" . "Lichner, \u013D." . . "P(IBS2060104), P(KSK3046108), P(SE/610/3/00), Z(AV0Z2060917)" . "Pra\u017E\u00E1k, Josef" . "V mal\u00E9m povod\u00ED byly pozorov\u00E1ny dva anom\u00E1ln\u00ED jevy: 1) v n\u011Bkter\u00FDch situac\u00EDch zp\u016Fsobila voda dodan\u00E1 z de\u0161t\u011B z\u0159eteln\u00FD pokles p\u016Fdn\u00ED vlhkosti. 2) V t\u011Bchto obdob\u00EDch m\u016F\u017Ee b\u00FDt pohyb p\u016Fdn\u00ED vl\u00E1hy vysv\u011Btlen pouze za p\u0159edpokladu oscila\u010Dn\u00EDho v\u00FDtoku p\u016Fdn\u00ED vody pod p\u016Fdn\u00ED profil. V t\u011Bchto situac\u00EDch prot\u00E9k\u00E1 velk\u00E9 mno\u017Estv\u00ED vody p\u016Fdou; proto tento jev v hydrologick\u00E9m m\u011B\u0159\u00EDtku tvo\u0159\u00ED velkou \u010D\u00E1st odtoku z povod\u00ED"@cs . "ES - \u0160pan\u011Blsk\u00E9 kr\u00E1lovstv\u00ED" . . "147;156" . "Instability driven flow and runoff formation in a small catchment" . "Tesa\u0159, Miroslav" . . "568353" . "3"^^ . "Instability driven flow and runoff formation in a small catchment" . . . "10"^^ . . "Instability driven flow and runoff formation in a small catchment"@en . . "RIV/67985874:_____/04:00104394!RIV/2005/AV0/A11005/N" . "Two anomalous phenomena were observed in a small catchment: 1) In some situations, the water supplied by rain caused a pronounced decrease in the soil water content. 2) In these periods, the soil water movement could be explained only by assuming an irregularly oscillating outflow of soil water into lower horizons. In these situations a large volume of water flows through the soil; therefore, on the hydrological scale, this phenomenon forms a great part of the outflow from a watershed" . "Instability driven flow and runoff formation in a small catchment"@en . "1"^^ . . . "Two anomalous phenomena were observed in a small catchment: 1) In some situations, the water supplied by rain caused a pronounced decrease in the soil water content. 2) In these periods, the soil water movement could be explained only by assuming an irregularly oscillating outflow of soil water into lower horizons. In these situations a large volume of water flows through the soil; therefore, on the hydrological scale, this phenomenon forms a great part of the outflow from a watershed"@en . "Geologica Acta" . . . "2" . . . "[28E8A2BD2505]" . "RIV/67985874:_____/04:00104394" . "2" .