About: The effect of earthworms and other saprophagous macrofauna on soil microstructure in reclaimed and un-reclaimed post-mining sites in Central Europe     Goto   Sponge   NotDistinct   Permalink

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Description
  • Studie porovnává densitu půdní makrofauny a struktur produkovaných půdní makrofaunou na rekultivovaných a nerekultivovaných plochách. Makrofauna a zejména žížaly jsou hojnější na rekultivovaných plochách, což vede k rychlejší tvorbě humusové vrstvy půdy. Tento rozdíl je výrazný zejména u mladých ploch, u ploch starých 40 let a starších se žížaly vyskytují i na nerekultivovaných plochách a rozdíl v půdní mikrostruktuře se zmenšuje. (cs)
  • Soil macrofauna density and the distribution of macrofauna faeces and other structures in topsoil were studied in two chronosequences of post-mining sites, the first overgrown by spontaneously developed vegetation and the second reclaimed by planting alder. Each chronosequence cosisted of three plots of the respective age of 15, 23 and 40 years since heaping. Density of all macrofauna groups, and earthworms in particular, was higher in reclaimed than in un-reclaimed sites. Soil microstructure formation was closely related to soil fauna density and activity. Faster earthworm colonization resulted in more rapid accumulation of earthworm coprolites in topsoil and consequent formation of humus layer in reclaimed than in un-reclaimed sites. Low density of earthworms in intermediate succession stages of un-reclaimed sites resulted in low soil mixing and in accumulation of litter fragments and macrofauna faecal pellets in soil surface, where they formed a massive fermentation layer.
  • Soil macrofauna density and the distribution of macrofauna faeces and other structures in topsoil were studied in two chronosequences of post-mining sites, the first overgrown by spontaneously developed vegetation and the second reclaimed by planting alder. Each chronosequence cosisted of three plots of the respective age of 15, 23 and 40 years since heaping. Density of all macrofauna groups, and earthworms in particular, was higher in reclaimed than in un-reclaimed sites. Soil microstructure formation was closely related to soil fauna density and activity. Faster earthworm colonization resulted in more rapid accumulation of earthworm coprolites in topsoil and consequent formation of humus layer in reclaimed than in un-reclaimed sites. Low density of earthworms in intermediate succession stages of un-reclaimed sites resulted in low soil mixing and in accumulation of litter fragments and macrofauna faecal pellets in soil surface, where they formed a massive fermentation layer. (en)
Title
  • The effect of earthworms and other saprophagous macrofauna on soil microstructure in reclaimed and un-reclaimed post-mining sites in Central Europe
  • The effect of earthworms and other saprophagous macrofauna on soil microstructure in reclaimed and un-reclaimed post-mining sites in Central Europe (en)
  • Vliv žížal a ostatní saprofágní makrofauny na půdní mikrostrukturu rekultivovaných a nerekultivovaných ploch po těžbě uhlí ve střední Evropě (cs)
skos:prefLabel
  • The effect of earthworms and other saprophagous macrofauna on soil microstructure in reclaimed and un-reclaimed post-mining sites in Central Europe
  • The effect of earthworms and other saprophagous macrofauna on soil microstructure in reclaimed and un-reclaimed post-mining sites in Central Europe (en)
  • Vliv žížal a ostatní saprofágní makrofauny na půdní mikrostrukturu rekultivovaných a nerekultivovaných ploch po těžbě uhlí ve střední Evropě (cs)
skos:notation
  • RIV/60077344:_____/07:00092111!RIV08-AV0-60077344
http://linked.open.../vavai/riv/strany
  • S184;S189
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(1QS600660505), P(GA526/01/1055), P(GA526/03/1259), P(GA526/06/0728), Z(AV0Z60660521)
http://linked.open...iv/cisloPeriodika
  • Suppl. 1
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 418906
http://linked.open...ai/riv/idVysledku
  • RIV/60077344:_____/07:00092111
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • earthworms; soil macrofauna; soil microstructure (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • FR - Francouzská republika
http://linked.open...ontrolniKodProRIV
  • [B1AC6A38E556]
http://linked.open...i/riv/nazevZdroje
  • European Journal of Soil Biology
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 43
http://linked.open...iv/tvurceVysledku
  • Frouz, Jan
  • Pižl, Václav
  • Tajovský, Karel
http://linked.open...n/vavai/riv/zamer
issn
  • 1164-5563
number of pages
is http://linked.open...avai/riv/vysledek of
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