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  • This paper evaluates different technologies of soil cultivation (conventional and minimization) in terms of physical properties and water regime of soils, where infiltration of surface water is a major component of subsurface water. Soil physical properties (the current humidity, reduced bulk density, porosity, water retention capacity of soil, pore distribution and soil aeration) is determined from soil samples taken from the organic horizon according to standard methodology. To observe the infiltration characteristics of surface layers of topsoil, the drench method (double ring infiltromctcrs) was used. For the evaluation of field measurements of infiltration, empirical and physically derived equations by Kostiakov and Philip and the three-parameter Philip-type equation were used. The Philip three-parameter equation provides physical based parameters near the theoretical values, a good estimation of saturated hydraulic conductivity Ks and sorptivity C, The parameter S of Philip's equation describes the real value of the sorptivity of the soil. Experimental research work on the experimental plots H. Meziricko proceeded in the years 2005-2008.
  • This paper evaluates different technologies of soil cultivation (conventional and minimization) in terms of physical properties and water regime of soils, where infiltration of surface water is a major component of subsurface water. Soil physical properties (the current humidity, reduced bulk density, porosity, water retention capacity of soil, pore distribution and soil aeration) is determined from soil samples taken from the organic horizon according to standard methodology. To observe the infiltration characteristics of surface layers of topsoil, the drench method (double ring infiltromctcrs) was used. For the evaluation of field measurements of infiltration, empirical and physically derived equations by Kostiakov and Philip and the three-parameter Philip-type equation were used. The Philip three-parameter equation provides physical based parameters near the theoretical values, a good estimation of saturated hydraulic conductivity Ks and sorptivity C, The parameter S of Philip's equation describes the real value of the sorptivity of the soil. Experimental research work on the experimental plots H. Meziricko proceeded in the years 2005-2008. (en)
Title
  • Evaluation of soil conservation technologies from the perspective of selected physical soil properties and infiltration capacity of the soil
  • Evaluation of soil conservation technologies from the perspective of selected physical soil properties and infiltration capacity of the soil (en)
skos:prefLabel
  • Evaluation of soil conservation technologies from the perspective of selected physical soil properties and infiltration capacity of the soil
  • Evaluation of soil conservation technologies from the perspective of selected physical soil properties and infiltration capacity of the soil (en)
skos:notation
  • RIV/00027049:_____/11:#0000462!RIV12-MZE-00027049
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(QH72203)
http://linked.open...iv/cisloPeriodika
  • 1
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
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  • 198360
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  • RIV/00027049:_____/11:#0000462
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  • soil conservation technologies; soil physical properties; infiltration capacity (en)
http://linked.open.../riv/klicoveSlovo
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  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [ABFC7CE5DB4F]
http://linked.open...i/riv/nazevZdroje
  • Acta universitatis agriculturae et silviculturae Mendeliane Brunensis
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  • 59
http://linked.open...iv/tvurceVysledku
  • Dumbrovský, Miroslav
  • Podhrázská, Jana
  • Pavlík, František
  • Kameníčková, Ivana
issn
  • 1211-8516
number of pages
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