Moisture conditions of the soil in spruce ecosystem in Oravská Polhora-Borsučie in growing seasons of 2012 and 2013
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41320%2F15%3AN0000033" target="_blank" >RIV/60460709:41320/15:N0000033 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.11118/beskyd201508010027" target="_blank" >http://dx.doi.org/10.11118/beskyd201508010027</a>
DOI - Digital Object Identifier
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Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Moisture conditions of the soil in spruce ecosystem in Oravská Polhora-Borsučie in growing seasons of 2012 and 2013
Popis výsledku v původním jazyce
The paper presents the research results of soil water regime under the spruce stand in the Upper Orava, in Oravská Polhora - Borsučie in the growing seasons of 2012 and 2013. There are characterized different ranges of soil moisture, soil water categories and its accessibility for plants, particularly for the surface layer from 20 cm to 100 cm deep physiological soil profile. Dominant interval of moisture during the growing season is the semiuvidic interval with the soil moisture between hydrolimits MCC and PDA. Amount of water presents mostly capillary less moving water, in the surface layer of soil sufficient, for short time insufficient supply of usable water. The amount of water decreseases for a short time after dry days. Semiaridic interval with the soil moisture between hydrolimits PDA and WP, up to the upper third of the variation range means that the vegetation has available stationary capillary water in the surface layer. In prolonged dry season such humidity condition can be one of the main causes of physiological weakening of spruce.
Název v anglickém jazyce
Moisture conditions of the soil in spruce ecosystem in Oravská Polhora-Borsučie in growing seasons of 2012 and 2013
Popis výsledku anglicky
The paper presents the research results of soil water regime under the spruce stand in the Upper Orava, in Oravská Polhora - Borsučie in the growing seasons of 2012 and 2013. There are characterized different ranges of soil moisture, soil water categories and its accessibility for plants, particularly for the surface layer from 20 cm to 100 cm deep physiological soil profile. Dominant interval of moisture during the growing season is the semiuvidic interval with the soil moisture between hydrolimits MCC and PDA. Amount of water presents mostly capillary less moving water, in the surface layer of soil sufficient, for short time insufficient supply of usable water. The amount of water decreseases for a short time after dry days. Semiaridic interval with the soil moisture between hydrolimits PDA and WP, up to the upper third of the variation range means that the vegetation has available stationary capillary water in the surface layer. In prolonged dry season such humidity condition can be one of the main causes of physiological weakening of spruce.
Klasifikace
Druh
O - Ostatní výsledky
CEP obor
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OECD FORD obor
40102 - Forestry
Návaznosti výsledku
Projekt
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Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2015
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů