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  • Na vybraných 140 lokalitách orných půd v ČR byl sledován obsah celkového organického C a jeho rozložitelné části. Ve více než 80% půdních vzorků se celkový obsah C pohyboval mezi 1 a 2 %. V lokalitách sledovaných v rámci Basálního monitoringu zemědělských půd, u kterých byl obsah celkového C sledován od roku 1992 nedošlo v uplynulém období k výrazným změnám. V Luvisolech a Albeluvisolech byl obsah C nižší než v Kambisolech, kde však byla vyšší variabilita této hodnoty. Obsah rozložitelného C v půdě koreloval s celkovým obsahem C. Nejnižší obsah rozložitelného C byl zjištěn v Luvisolech, zřejmě v důsledku vhodných podmínek pro mikrobní aktivitu a přeměny organické hmoty. Obsah horkou vodou extrahovatelného C činil 3 – 4 % celkového C. (cs)
  • Total soil organic matter and its decomposable part have been studied in arable farm fields in the Czech Republic. Organic C content in the top soil from the selected 140 sites on arable soils ranged between 1% and 2% in more than 80% of the soil samples. C/N ratio oscillated around 10 in a rather narrow band. There were no remarkable changes in the organic C content in the top soil in 82 sites over the last decade (1992 to 2002). The distribution of the organic C content in the soil samples according to the taxonomical soil units have shown the lowest values in the Haplic Luvisols and Albeluvisols. Their variability was relatively low. In Cambisols, on the contrary, the average C content values were higher but their variability was also much higher than in Luvisols. The decomposable organic C content closely correlated with the total organic C content. The lowest decomposable C contents were found in the soil samples from Luvisols, probably due to the favourable conditions for microbial activities a
  • Total soil organic matter and its decomposable part have been studied in arable farm fields in the Czech Republic. Organic C content in the top soil from the selected 140 sites on arable soils ranged between 1% and 2% in more than 80% of the soil samples. C/N ratio oscillated around 10 in a rather narrow band. There were no remarkable changes in the organic C content in the top soil in 82 sites over the last decade (1992 to 2002). The distribution of the organic C content in the soil samples according to the taxonomical soil units have shown the lowest values in the Haplic Luvisols and Albeluvisols. Their variability was relatively low. In Cambisols, on the contrary, the average C content values were higher but their variability was also much higher than in Luvisols. The decomposable organic C content closely correlated with the total organic C content. The lowest decomposable C contents were found in the soil samples from Luvisols, probably due to the favourable conditions for microbial activities a (en)
Title
  • Total organic C and its decomposable part in arable soils in the Czech republic
  • Total organic C and its decomposable part in arable soils in the Czech republic (en)
  • Celkový obsah C a jeho rozložitelné části v orných půdách ČR (cs)
skos:prefLabel
  • Total organic C and its decomposable part in arable soils in the Czech republic
  • Total organic C and its decomposable part in arable soils in the Czech republic (en)
  • Celkový obsah C a jeho rozložitelné části v orných půdách ČR (cs)
skos:notation
  • RIV/00027006:_____/04:2428!RIV08-MZE-00027006
http://linked.open.../vavai/riv/strany
  • 21;32
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  • P(QD1329)
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  • 1
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  • 590492
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  • RIV/00027006:_____/04:2428
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  • Soil organic matter; decomposable soil orgaic matter; organic carbon; hot water souluble carbon; inert organic carbon (en)
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http://linked.open...odStatuVydavatele
  • CZ - Česká republika
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  • [867EDEDB2BAC]
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  • neuveden
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  • 50
http://linked.open...iv/tvurceVysledku
  • Cerhanová, Dana
  • Nováková, Jitka
  • Dostál, J.
  • Kubát, Jaromír
  • Klement, V.
  • Čermák, P.
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