Hydrological regime and physico-chemical water properties of various types of peat bog sites: Case study of Mezilesní peat bog, Šumava Mts.
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F46747885%3A24510%2F20%3A00008675" target="_blank" >RIV/46747885:24510/20:00008675 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/00216208:11310/20:10414190
Výsledek na webu
<a href="https://doi.org/10.37040/geografie2020125010021" target="_blank" >https://doi.org/10.37040/geografie2020125010021</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.37040/geografie2020125010021" target="_blank" >10.37040/geografie2020125010021</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Hydrological regime and physico-chemical water properties of various types of peat bog sites: Case study of Mezilesní peat bog, Šumava Mts.
Popis výsledku v původním jazyce
In a period with frequently occurring hydrological extremes, research on areas with a high retention potential is brought into focus. The Šumava Mountains peat bogs are important parts of the landscape in the headwater area of the Otava river basin. The study objective is to describe the variability of discharges and the dynamics of groundwater level changes in various types of peat bogs, and to identify connections between observed physico-chemical water properties. This is assessed by basic statistical methods. The rainfall-runoff process and physico-chemical water properties can be affected by many factors. In this case, strong relations between the observed parameters were identified along with considerable differences in the involvement of various types of peat bog sites in the runoff process. It is evident that the peat bog pattern and its vegetation cover have an essential effect on the hydrological regime and water properties stored in a peat bog.
Název v anglickém jazyce
Hydrological regime and physico-chemical water properties of various types of peat bog sites: Case study of Mezilesní peat bog, Šumava Mts.
Popis výsledku anglicky
In a period with frequently occurring hydrological extremes, research on areas with a high retention potential is brought into focus. The Šumava Mountains peat bogs are important parts of the landscape in the headwater area of the Otava river basin. The study objective is to describe the variability of discharges and the dynamics of groundwater level changes in various types of peat bogs, and to identify connections between observed physico-chemical water properties. This is assessed by basic statistical methods. The rainfall-runoff process and physico-chemical water properties can be affected by many factors. In this case, strong relations between the observed parameters were identified along with considerable differences in the involvement of various types of peat bog sites in the runoff process. It is evident that the peat bog pattern and its vegetation cover have an essential effect on the hydrological regime and water properties stored in a peat bog.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10508 - Physical geography
Návaznosti výsledku
Projekt
—
Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2020
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Geografie
ISSN
1212-0014
e-ISSN
—
Svazek periodika
125
Číslo periodika v rámci svazku
1
Stát vydavatele periodika
CZ - Česká republika
Počet stran výsledku
26
Strana od-do
21-46
Kód UT WoS článku
000567346600002
EID výsledku v databázi Scopus
2-s2.0-85087095060