Počet záznamů: 1
Behavior of spring discharge dynamic at forest and grassland mountain catchments
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SYSNO ASEP 0090712 Druh ASEP A - Abstrakt Zařazení RIV Záznam nebyl označen do RIV Zařazení RIV Není vybrán druh dokumentu Název Behavior of spring discharge dynamic at forest and grassland mountain catchments Překlad názvu Behavior of spring discharge dynamic at forest and grassland mountain catchmentsDynamika jarních odtoků z pramene v horském lesním a lučním povodí Tvůrce(i) Pavelka, Marian (UEK-B) RID, ORCID, SAI
Acosta, Manuel (UEK-B) RID, ORCID, SAI
Janouš, Dalibor (UEK-B) RID, SAI
Czerný, Radek (UEK-B) ORCID, SAI
Tomášková, Ivana (UEK-B)Zdroj.dok. The Beskyds Buletin - ISBN 978-80-7375-069-5
Roč. 1, č. 20 (2007), s. 55-60Poč.str. 6 s. Jazyk dok. eng - angličtina Země vyd. CZ - Česká republika Klíč. slova precipitation ; spring discharge ; evapotranspiration ; Norway spruce ; grassland ; roots Vědní obor RIV GK - Lesnictví CEP 1P05OC027 GA MŠMT - Ministerstvo školství, mládeže a tělovýchovy CEZ AV0Z60870520 - UEK-B (2005-2011) Anotace In this study we measured precipitation, spring discharge and evapotranspiration in order to explain the existence of diurnal oscillation of spring discharge presented at forest stand catchment and its comparison with grassland spring discharge. Measurements were carried out in forest stand and a grassland site at the Ecological Experimental Study Site Bily Kriz, Moravian-Silesian Beskydy Mts., the Czech Republic. Even thought, precipitation at the forest and the grassland sites were without significant differences and both spring are of the same type, difference between courses of spring discharge were found during the period after raining. Our time series analysis supported the hypothesis that the forest spring discharge oscillation responds to the evapotranspiration. Překlad anotace In this study we measured precipitation, spring discharge and evapotranspiration in order to explain the existence of diurnal oscillation of spring discharge presented at forest stand catchment and its comparison with grassland spring discharge. Measurements were carried out in forest stand and a grassland site at the Ecological Experimental Study Site Bily Kriz, Moravian-Silesian Beskydy Mts., the Czech Republic. Even thought, precipitation at the forest and the grassland sites were without significant differences and both spring are of the same type, difference between courses of spring discharge were found during the period after raining. Our time series analysis supported the hypothesis that the forest spring discharge oscillation responds to the evapotranspiration. Pracoviště Ústav výzkumu globální změny Kontakt Nikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268 Rok sběru 2008
Počet záznamů: 1