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  • Agricultural lands in foothill zones on acid crystalline rocks can be an important source of diffused nitrate pollution affecting the quality of both subsurface and surface waters. Field experiment established to optimise the drip irrigation of potatoes was set up in the highland region. The soil is a deep loamy Planosol. It has capacity to swell and shrink and contains macropores. An attempt is made to explain the major part of the measured spatial variability of soil water pressure by means of dual permeability modelling. S1D DUAL model was used to simulate seasonal soil water suction variations. Inverse modelling was applied in order to minimize the discrepancies between the model responses and observed pressure heads. Levenberg-Marquardt algorithm, was used as a parameter estimator. It is concluded that the measurements of soil water pressure provide valuable information about the physical nature of water flow, and can help us to quantify parameters of dual permeability models.
  • Agricultural lands in foothill zones on acid crystalline rocks can be an important source of diffused nitrate pollution affecting the quality of both subsurface and surface waters. Field experiment established to optimise the drip irrigation of potatoes was set up in the highland region. The soil is a deep loamy Planosol. It has capacity to swell and shrink and contains macropores. An attempt is made to explain the major part of the measured spatial variability of soil water pressure by means of dual permeability modelling. S1D DUAL model was used to simulate seasonal soil water suction variations. Inverse modelling was applied in order to minimize the discrepancies between the model responses and observed pressure heads. Levenberg-Marquardt algorithm, was used as a parameter estimator. It is concluded that the measurements of soil water pressure provide valuable information about the physical nature of water flow, and can help us to quantify parameters of dual permeability models. (en)
  • Inverzní modelování dynamiky půdní vody v heterogenní půdě s makropóry (cs)
Title
  • Inverse Modelling of Soil Water Dynamics in Heterogeneous Soil with Macropores
  • Inverse Modelling of Soil Water Dynamics in Heterogeneous Soil with Macropores (en)
  • Inverzní modelování dynamiky půdní vody v heterogenní půdě s makropóry (cs)
skos:prefLabel
  • Inverse Modelling of Soil Water Dynamics in Heterogeneous Soil with Macropores
  • Inverse Modelling of Soil Water Dynamics in Heterogeneous Soil with Macropores (en)
  • Inverzní modelování dynamiky půdní vody v heterogenní půdě s makropóry (cs)
skos:notation
  • RIV/68407700:21110/05:01116866!RIV06-GA0-21110___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA103/04/0663)
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
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  • 525578
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  • RIV/68407700:21110/05:01116866
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • dual-permeability model; inverse modelling (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...i/riv/kodPristupu
http://linked.open...ontrolniKodProRIV
  • [77D12EC3D597]
http://linked.open...i/riv/mistoVydani
  • Katlenburg-Lindau
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  • neuvedeno
http://linked.open...in/vavai/riv/obor
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http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...iv/tvurceVysledku
  • Císlerová, Milena
  • Dohnal, Michal
  • Doležal, František
  • Dušek, Jaromír
  • Vogel, Tomáš
http://localhost/t...ganizacniJednotka
  • 21110
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