Detrital components in submontane organogenic springs in relation to their morphology, microhabitats and macroinvertebrates
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00020711%3A_____%2F12%3A00003750" target="_blank" >RIV/00020711:_____/12:00003750 - isvavai.cz</a>
Výsledek na webu
<a href="http://ets.webofknowledge.com/ETS/saveDataToFile.do" target="_blank" >http://ets.webofknowledge.com/ETS/saveDataToFile.do</a>
DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Detrital components in submontane organogenic springs in relation to their morphology, microhabitats and macroinvertebrates
Popis výsledku v původním jazyce
Fine particulate organic matter (FPOM), originated by aggregation of smaller particles and by decomposition of bigger particles, usually presents the dominant energy and nutrient source in the primary river net. Relationships between detrital components,environmental factors and macroinvertebrate composition were investigated in 52 submontane organogenic spring areas in small catchment in the Šumava foothills, Czech Republic. All three types of springs (helocrenes, rheocrenes and limnocrenes) were represented, as well as springs with the transitional character. The selected springs were permanent, with water discharge higher than 0.1 L s-1, they all were coldwater and stenothermic, with the winter water temperature at the point of the source ranging from 2.0 to 9.9°C. At each spring area, the main morphological and physical characteristics of the spring and surrounding area were recorded.
Název v anglickém jazyce
Detrital components in submontane organogenic springs in relation to their morphology, microhabitats and macroinvertebrates
Popis výsledku anglicky
Fine particulate organic matter (FPOM), originated by aggregation of smaller particles and by decomposition of bigger particles, usually presents the dominant energy and nutrient source in the primary river net. Relationships between detrital components,environmental factors and macroinvertebrate composition were investigated in 52 submontane organogenic spring areas in small catchment in the Šumava foothills, Czech Republic. All three types of springs (helocrenes, rheocrenes and limnocrenes) were represented, as well as springs with the transitional character. The selected springs were permanent, with water discharge higher than 0.1 L s-1, they all were coldwater and stenothermic, with the winter water temperature at the point of the source ranging from 2.0 to 9.9°C. At each spring area, the main morphological and physical characteristics of the spring and surrounding area were recorded.
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
EH - Ekologie – společenstva
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
Z - Vyzkumny zamer (s odkazem do CEZ)
Ostatní
Rok uplatnění
2012
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Polish Journal of Ecology
ISSN
1505-2249
e-ISSN
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Svazek periodika
2012
Číslo periodika v rámci svazku
60
Stát vydavatele periodika
CZ - Česká republika
Počet stran výsledku
13
Strana od-do
163-175
Kód UT WoS článku
000301696500013
EID výsledku v databázi Scopus
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