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Statements

Subject Item
n2:RIV%2F62156489%3A43410%2F09%3A00141394%21RIV09-MSM-43410___
rdf:type
skos:Concept n12:Vysledek
dcterms:description
To better understand the chemical transformation of the rainfall after the passage through the canopies it is necessary to study throughfall deposition fluxes within forest stands. The comparison of bulk deposition fluxes of Ca, Mg, K, S-SO4, N-NO3 and N-NH4 within the mountain spruce stands with different stand density and bulk deposition fluxes on the open area was made at the study site of Bílý Kříž (Moravian-Silesian Beskids Mts., the Czech Republic) during the period of 1999-2006. Linear relationship between the amount of rainfall on the open area and the amount of throughfall within the spruce stand was found. Throughfall deposition fluxes of selected elements within the dense as well as within the sparse spruce stands were higher when compared with bulk deposition fluxes on the open area. Mostly there were statistical significant differences between the bulk deposition fluxes on the open area and within the studied spruce stands. The throughfall deposition fluxes of Ca, Mg, K and S-SO4 were inf To better understand the chemical transformation of the rainfall after the passage through the canopies it is necessary to study throughfall deposition fluxes within forest stands. The comparison of bulk deposition fluxes of Ca, Mg, K, S-SO4, N-NO3 and N-NH4 within the mountain spruce stands with different stand density and bulk deposition fluxes on the open area was made at the study site of Bílý Kříž (Moravian-Silesian Beskids Mts., the Czech Republic) during the period of 1999-2006. Linear relationship between the amount of rainfall on the open area and the amount of throughfall within the spruce stand was found. Throughfall deposition fluxes of selected elements within the dense as well as within the sparse spruce stands were higher when compared with bulk deposition fluxes on the open area. Mostly there were statistical significant differences between the bulk deposition fluxes on the open area and within the studied spruce stands. The throughfall deposition fluxes of Ca, Mg, K and S-SO4 were inf Studium depozičních toků v lesních porostech je důležité pro pochopení chemických změn, ke kterým dochází při průchodu srážek korunovou vrstvou porostů. V letech 1999-2006 byly sledovány depoziční toky Ca, Mg, K, S-SO4, N-NO3 a N-NH4 v horském smrkovém porostu na dvou plochách s různou hustotou a na volné ploše na experimentálním ekologickém pracovišti Bílý Kříž (Moravskoslezské Beskydy). Byla zjištěna lineární závislost mezi množstvím srážek dopadajících na volnou plochu a množstvím podkorunových srážek na obou studovaných plochách. Podkorunové depoziční toky vybraných prvků byly ve sledovaném období 1999-2006 vyšší ve smrkových porostech než depoziční toky na volné ploše. Pro většinu vybraných prvků byly zjištěny statisticky významné rozdíly mezi depozičními toky na volné ploše a ve studovaných smrkových porostech. Depoziční toky Ca, Mg, K a S-SO4 byly ve smrkovém porostu ovlivněny jeho hustotou.
dcterms:title
Comparison of deposition fluxes on the open area and in mountain spruce stands of different density Comparison of deposition fluxes on the open area and in mountain spruce stands of different density Srovnání depozičních toků na volné ploše a ve smrkových porostech s různou hustotou
skos:prefLabel
Comparison of deposition fluxes on the open area and in mountain spruce stands of different density Comparison of deposition fluxes on the open area and in mountain spruce stands of different density Srovnání depozičních toků na volné ploše a ve smrkových porostech s různou hustotou
skos:notation
RIV/62156489:43410/09:00141394!RIV09-MSM-43410___
n5:aktivita
n17:Z
n5:aktivity
Z(MSM6215648902)
n5:cisloPeriodika
9
n5:dodaniDat
n11:2009
n5:domaciTvurceVysledku
n7:4930231 n7:3354415 n7:1131451
n5:druhVysledku
n15:J
n5:duvernostUdaju
n18:S
n5:entitaPredkladatele
n14:predkladatel
n5:idSjednocenehoVysledku
307698
n5:idVysledku
RIV/62156489:43410/09:00141394
n5:jazykVysledku
n9:eng
n5:klicovaSlova
throughfall; Norway spruce; Moravian-Silesian Beskids Mts.; Czech Republic
n5:klicoveSlovo
n8:throughfall n8:Czech%20Republic n8:Norway%20spruce n8:Moravian-Silesian%20Beskids%20Mts.
n5:kodStatuVydavatele
CZ - Česká republika
n5:kontrolniKodProRIV
[20A294D124F8]
n5:nazevZdroje
Journal of Forest Science
n5:obor
n16:GK
n5:pocetDomacichTvurcuVysledku
3
n5:pocetTvurcuVysledku
3
n5:rokUplatneniVysledku
n11:2009
n5:svazekPeriodika
55
n5:tvurceVysledku
Drápelová, Ida Marková, Irena Truparová, Sabina
n5:zamer
n6:MSM6215648902
s:issn
1212-4834
s:numberOfPages
8
n10:organizacniJednotka
43410