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  • The adsorption isotherms were obtained for two horizons (humus horizon and subsurface horizon) of six various soil types of the Czech Republic using a standard laboratory procedure. The Freundlich and Langmuir equations were used to fit data points of the adsorption isotherms. The adsorption isotherms of the humus horizons significantly differ from the adsorption isotherms of the horizons below the humus horizons that is caused by different soil properties. The adsorption isotherms obtained on the soil samples taken in different years slightly differs. The reason may be seasonal soil property changes and heterogeneity. The chlorotoluron mobility characterized by the adsorption isotherms corresponds with the chlorotoluron mobility observed in the field in 2004 (Kočárek et al., 2005a,b). Therelationship between prameters of both absorption isotherms and soil properties like clay content, pHKCl, organic carbon, cation exchange capacity, was studied. As was expected adsorption process in studied soils is
  • The adsorption isotherms were obtained for two horizons (humus horizon and subsurface horizon) of six various soil types of the Czech Republic using a standard laboratory procedure. The Freundlich and Langmuir equations were used to fit data points of the adsorption isotherms. The adsorption isotherms of the humus horizons significantly differ from the adsorption isotherms of the horizons below the humus horizons that is caused by different soil properties. The adsorption isotherms obtained on the soil samples taken in different years slightly differs. The reason may be seasonal soil property changes and heterogeneity. The chlorotoluron mobility characterized by the adsorption isotherms corresponds with the chlorotoluron mobility observed in the field in 2004 (Kočárek et al., 2005a,b). Therelationship between prameters of both absorption isotherms and soil properties like clay content, pHKCl, organic carbon, cation exchange capacity, was studied. As was expected adsorption process in studied soils is (en)
  • The adsorption isotherms were obtained for two horizons (humus horizon and subsurface horizon) of six various soil types of the Czech Republic using a standard laboratory procedure. The Freundlich and Langmuir equations were used to fit data points of the adsorption isotherms. The adsorption isotherms of the humus horizons significantly differ from the adsorption isotherms of the horizons below the humus horizons that is caused by different soil properties. The adsorption isotherms obtained on the soil samples taken in different years slightly differs. The reason may be seasonal soil property changes and heterogeneity. The chlorotoluron mobility characterized by the adsorption isotherms corresponds with the chlorotoluron mobility observed in the field in 2004 (Kočárek et al., 2005a,b). Therelationship between prameters of both absorption isotherms and soil properties like clay content, pHKCl, organic carbon, cation exchange capacity, was studied. As was expected adsorption process in studied soils is (cs)
Title
  • Estimation of parameters describing Freundlich and Langmuir adsorption isotherm
  • Estimation of parameters describing Freundlich and Langmuir adsorption isotherm (en)
  • Odhad parametrů vyjadřujících Freunlichovu a Langmuirovu adsorpční izotermu. (cs)
skos:prefLabel
  • Estimation of parameters describing Freundlich and Langmuir adsorption isotherm
  • Estimation of parameters describing Freundlich and Langmuir adsorption isotherm (en)
  • Odhad parametrů vyjadřujících Freunlichovu a Langmuirovu adsorpční izotermu. (cs)
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  • RIV/60460709:41210/05:10758!RIV06-GA0-41210___
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  • solution transport, herbicide, adsorption isotherm, clay content, pHKCl, organic carbon, cation exchange capacity, Freundlich and Langmuir adsorption isotherms (en)
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  • 13th International Poster Day Transport of Water, Chemicals and Energy in the System Soil Crop Canopy-Atmosphere
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  • Kodešová, Radka
  • Kočárek, Martin
  • Kozák, Josef
  • Pijálková, Helena
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  • Ústav hydrológie SAV; Geofyzikálny ústav SAV
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  • 41210
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