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Description
  • Se vzrůstem kompresního napětí dochází ke snížení celkové pórovitosti půdy. Mnohem významnější však je snížení strukturální pórovitosti. Poměrná hodnota snížení strukturální pórovitosti v důsledku komprese byla v rozmezí 0,91 až 0,48. Změna matriční pórovitosti neměla stejnou tendenci ve všech půdách. Ve většině půd a testů matriční pórovitost vzrůstala se vzrůstem kompresního napětí. Charakteristiky distribuční funkce velikosti pórů se neměnily uniformně. Obecné pravidlo změny distribuční funkce nebylo nalezeno. Změna závisela na půdním taxonu, stabilitě struktury a na prekompresním napětí. (cs)
  • The increase of the compression stress caused a decrease of the total porosity, but the decrease of the structural porosity was much more expressed. The ratio of the decrease of structural porosity due to compression was in ranges between 0.91 and 0.48. The change of the matrix porosity has not the same tendency in all soils. In majority of instances it was increasing with the increase of compression stress. The characteristics of the pore size distribution did not change in a uniform way. A generally valid rule on the change of the pore size distribution due to compression does not exist. The change depends upon the soil taxon, the structural stability and upon the precompression stress.
  • The increase of the compression stress caused a decrease of the total porosity, but the decrease of the structural porosity was much more expressed. The ratio of the decrease of structural porosity due to compression was in ranges between 0.91 and 0.48. The change of the matrix porosity has not the same tendency in all soils. In majority of instances it was increasing with the increase of compression stress. The characteristics of the pore size distribution did not change in a uniform way. A generally valid rule on the change of the pore size distribution due to compression does not exist. The change depends upon the soil taxon, the structural stability and upon the precompression stress. (en)
Title
  • Vliv uniaxiální komprese na distribuční funkci velikosti pórů v bi-modálních půdách (cs)
  • The influence of uniaxial compression upon pore size distribution in bi-modal soils
  • The influence of uniaxial compression upon pore size distribution in bi-modal soils (en)
skos:prefLabel
  • Vliv uniaxiální komprese na distribuční funkci velikosti pórů v bi-modálních půdách (cs)
  • The influence of uniaxial compression upon pore size distribution in bi-modal soils
  • The influence of uniaxial compression upon pore size distribution in bi-modal soils (en)
skos:notation
  • RIV/25768654:_____/06:#0000001!RIV08-GA0-25768654
http://linked.open.../vavai/riv/strany
  • 27-37
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA103/05/2143)
http://linked.open...iv/cisloPeriodika
  • 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
  • 479572
http://linked.open...ai/riv/idVysledku
  • RIV/25768654:_____/06:#0000001
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Pore size distribution,Soil kompression, Bi-modal soils,Structural porosity, Soil water retention (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • NL - Nizozemsko
http://linked.open...ontrolniKodProRIV
  • [5132A99A172D]
http://linked.open...i/riv/nazevZdroje
  • Soil and Tillage Research
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
  • 86
http://linked.open...iv/tvurceVysledku
  • Kutílek, Miroslav
issn
  • 0167-1987
number of pages
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