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Statements

Subject Item
n2:RIV%2F61989100%3A27350%2F11%3A86078699%21RIV12-MSM-27350___
rdf:type
skos:Concept n6:Vysledek
dcterms:description
Three sites with a different type of vegetation (coniferous, deciduous and grass field) were chosen in the Moravian Karst for a soil sampling. Soil profiles were taken, divided into individual samples (each about 10 cm in a length of the soil profile, i.e., about 25 g of weight) and leached by distilled water and KCl solution (25 %). The pH was generally low near surface (A-horizon). Such low values suggest the presence of humic species. The pH-values do not change markedly along profiles from the locality with a grass cover. The pH-values of the leachates from the soils under deciduous vegetation stagnate to the depth of approximately 25 cm and steeply increase to the values of 7.02 below this horizon. In the soils under coniferous vegetation, pH gradually increases to the values of 5.61 /KCl solution/ and 6.81 in the profile depth of 75-85 cm. The systematically lower pH-values and deeper soil profiles under coniferous indicate that soil solutions under this type of vegetation are more aggressive. Three sites with a different type of vegetation (coniferous, deciduous and grass field) were chosen in the Moravian Karst for a soil sampling. Soil profiles were taken, divided into individual samples (each about 10 cm in a length of the soil profile, i.e., about 25 g of weight) and leached by distilled water and KCl solution (25 %). The pH was generally low near surface (A-horizon). Such low values suggest the presence of humic species. The pH-values do not change markedly along profiles from the locality with a grass cover. The pH-values of the leachates from the soils under deciduous vegetation stagnate to the depth of approximately 25 cm and steeply increase to the values of 7.02 below this horizon. In the soils under coniferous vegetation, pH gradually increases to the values of 5.61 /KCl solution/ and 6.81 in the profile depth of 75-85 cm. The systematically lower pH-values and deeper soil profiles under coniferous indicate that soil solutions under this type of vegetation are more aggressive.
dcterms:title
Acid-base reactions of karst soils in dependence on vegetation type Acid-base reactions of karst soils in dependence on vegetation type
skos:prefLabel
Acid-base reactions of karst soils in dependence on vegetation type Acid-base reactions of karst soils in dependence on vegetation type
skos:notation
RIV/61989100:27350/11:86078699!RIV12-MSM-27350___
n6:predkladatel
n7:orjk%3A27350
n3:aktivita
n11:S n11:V
n3:aktivity
S, V
n3:cisloPeriodika
1
n3:dodaniDat
n5:2012
n3:domaciTvurceVysledku
n16:2787393
n3:druhVysledku
n13:J
n3:duvernostUdaju
n14:S
n3:entitaPredkladatele
n8:predkladatel
n3:idSjednocenehoVysledku
184447
n3:idVysledku
RIV/61989100:27350/11:86078699
n3:jazykVysledku
n17:eng
n3:klicovaSlova
Moravian Karst; pH-values; vegetation; soil; karst; acid-base reaction
n3:klicoveSlovo
n10:Moravian%20Karst n10:soil n10:karst n10:vegetation n10:pH-values n10:acid-base%20reaction
n3:kodStatuVydavatele
SK - Slovenská republika
n3:kontrolniKodProRIV
[2085EDA84BC9]
n3:nazevZdroje
Slovenský kras (Acta Carsologica Slovaca)
n3:obor
n4:DD
n3:pocetDomacichTvurcuVysledku
1
n3:pocetTvurcuVysledku
3
n3:rokUplatneniVysledku
n5:2011
n3:svazekPeriodika
48
n3:tvurceVysledku
Ličbinská, Monika Hýlová, Lada Faimon, Jiří
s:issn
0560-3137
s:numberOfPages
6
n15:organizacniJednotka
27350