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Statements

Subject Item
n2:RIV%2F67985874%3A_____%2F10%3A00349887%21RIV11-MSM-67985874
rdf:type
n13:Vysledek skos:Concept
dcterms:description
Plant cover and surface crusts can influence soil hydrology considerably after long periods of hot weather and drought when water repellency (WR) is greatest. This was studied on an aeolian sandy soil that frequently experiences long dry and hot weather, followed by intense precipitation. The different vegetation covers examined were (1) predominantly grass species (grassland soil); (2) a 30-year-old Scots pine forest (forest soil); (3) mainly moss species (glade soil) and (4) subsoil at 50-cm depth of treatment (5) to remove the influence of vegetation or soil crusts (pure sand). Vegetation cover influenced hydrological and pedological properties of the sandy soil. Both the water drop penetration time (WDPT) and WR index R decreased in the order: forest soil - glade soil = grassland soil - pure sand. WDPT and R were up to 3 orders of magnitude greater, whereas sorptivity and hydraulic conductivity were up to 3 orders of magnitude less, in some vegetated soils compared to pure sand. Plant cover and surface crusts can influence soil hydrology considerably after long periods of hot weather and drought when water repellency (WR) is greatest. This was studied on an aeolian sandy soil that frequently experiences long dry and hot weather, followed by intense precipitation. The different vegetation covers examined were (1) predominantly grass species (grassland soil); (2) a 30-year-old Scots pine forest (forest soil); (3) mainly moss species (glade soil) and (4) subsoil at 50-cm depth of treatment (5) to remove the influence of vegetation or soil crusts (pure sand). Vegetation cover influenced hydrological and pedological properties of the sandy soil. Both the water drop penetration time (WDPT) and WR index R decreased in the order: forest soil - glade soil = grassland soil - pure sand. WDPT and R were up to 3 orders of magnitude greater, whereas sorptivity and hydraulic conductivity were up to 3 orders of magnitude less, in some vegetated soils compared to pure sand.
dcterms:title
Vegetation impact on the hydrology of an aeolian sandy soil in a continental climate Vegetation impact on the hydrology of an aeolian sandy soil in a continental climate
skos:prefLabel
Vegetation impact on the hydrology of an aeolian sandy soil in a continental climate Vegetation impact on the hydrology of an aeolian sandy soil in a continental climate
skos:notation
RIV/67985874:_____/10:00349887!RIV11-MSM-67985874
n3:aktivita
n14:P n14:Z
n3:aktivity
P(MEB0808114), Z(AV0Z20600510)
n3:cisloPeriodika
4
n3:dodaniDat
n7:2011
n3:domaciTvurceVysledku
n17:9271074 n17:3797732
n3:druhVysledku
n11:J
n3:duvernostUdaju
n18:S
n3:entitaPredkladatele
n5:predkladatel
n3:idSjednocenehoVysledku
295420
n3:idVysledku
RIV/67985874:_____/10:00349887
n3:jazykVysledku
n8:eng
n3:klicovaSlova
sandy soil; water repellency; plant cover; sorptivity; hydraulic conductivity
n3:klicoveSlovo
n9:water%20repellency n9:sorptivity n9:plant%20cover n9:hydraulic%20conductivity n9:sandy%20soil
n3:kodStatuVydavatele
US - Spojené státy americké
n3:kontrolniKodProRIV
[933F14252FF4]
n3:nazevZdroje
Ecohydrology
n3:obor
n15:DA
n3:pocetDomacichTvurcuVysledku
2
n3:pocetTvurcuVysledku
7
n3:projekt
n16:MEB0808114
n3:rokUplatneniVysledku
n7:2010
n3:svazekPeriodika
3
n3:tvurceVysledku
Lichner, Ľ. Hallett, P. D. Tesař, Miroslav Šír, Miloslav Orfánus, T. Rajkai, K. Czachor, H.
n3:wos
000285227700005
n3:zamer
n12:AV0Z20600510
s:issn
1936-0584
s:numberOfPages
8