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Statements

Subject Item
n2:RIV%2F00020699%3A_____%2F05%3A8P002990%21RIV08-MZE-00020699
rdf:type
skos:Concept n11:Vysledek
dcterms:description
The cumulative evapotranspiration of maize stand was determined during the growing season over the period of 148 days from planting to the full ripeness. The total evapotranspiration in this time interval was 276,4 mm while the amount of precipitation reached in the analysed period 295,4 mm. The transpiration and soil evaporation daily courses were calculated using a verified mathematical model of interrelationship existing within the system soil-plant-atmosphere. In the vegetation period 2000 the investigated maize stand transpirated under changing environmental conditions. It was found that soil water availability practically did not affect the evapotranspiration when at least 58,2% of extractable soil water was present in the root zone, but below this value, the evapotranspiration decreased linearly with the decrease in the soil water content. Ve vegetačním období 2000 studovaný porost kukuřice transpiroval v různých podmínkách prostředí a za významného poklesu půdní vlhkosti zaznamenané na konci června. Zjištěno bylo, že dostupnost půdní vody prakticky neovlivnila evapotranspiraci, pokud alespoň 58,2% extrahovatelné půdní vody bylo přítomno v kořenové zóně, ale pod touto hodnotou klesala evapotranspirace lineárně s poklesem obsahu půdní vody. The cumulative evapotranspiration of maize stand was determined during the growing season over the period of 148 days from planting to the full ripeness. The total evapotranspiration in this time interval was 276,4 mm while the amount of precipitation reached in the analysed period 295,4 mm. The transpiration and soil evaporation daily courses were calculated using a verified mathematical model of interrelationship existing within the system soil-plant-atmosphere. In the vegetation period 2000 the investigated maize stand transpirated under changing environmental conditions. It was found that soil water availability practically did not affect the evapotranspiration when at least 58,2% of extractable soil water was present in the root zone, but below this value, the evapotranspiration decreased linearly with the decrease in the soil water content.
dcterms:title
Effect of soil moisture on evapotranspiration of a maize stand during one growing season Effect of soil moisture on evapotranspiration of a maize stand during one growing season Vliv půdní vlhkosti na evapotranspiraci porostu kukuřice během vegetační doby
skos:prefLabel
Vliv půdní vlhkosti na evapotranspiraci porostu kukuřice během vegetační doby Effect of soil moisture on evapotranspiration of a maize stand during one growing season Effect of soil moisture on evapotranspiration of a maize stand during one growing season
skos:notation
RIV/00020699:_____/05:8P002990!RIV08-MZE-00020699
n4:strany
219-228
n4:aktivita
n12:P
n4:aktivity
P(QF3100)
n4:cisloPeriodika
3
n4:dodaniDat
n10:2008
n4:domaciTvurceVysledku
n15:8675309
n4:druhVysledku
n9:J
n4:duvernostUdaju
n7:S
n4:entitaPredkladatele
n17:predkladatel
n4:idSjednocenehoVysledku
519438
n4:idVysledku
RIV/00020699:_____/05:8P002990
n4:jazykVysledku
n14:eng
n4:klicovaSlova
maize; soil moisture; evapotranspiration
n4:klicoveSlovo
n8:maize n8:evapotranspiration n8:soil%20moisture
n4:kodStatuVydavatele
SK - Slovenská republika
n4:kontrolniKodProRIV
[0251B7873014]
n4:nazevZdroje
Contributions to Geophysics and Geodesy
n4:obor
n5:DG
n4:pocetDomacichTvurcuVysledku
1
n4:pocetTvurcuVysledku
3
n4:projekt
n16:QF3100
n4:rokUplatneniVysledku
n10:2005
n4:svazekPeriodika
35
n4:tvurceVysledku
Hurtalová, T. Rožnovský, Jaroslav Matejka, F.
s:issn
1335-2806
s:numberOfPages
10