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Description
  • Soil water and heat transport plays an important role in various hydrologic, agricultural, and industrial applications. Accordingly, an increasing attention is paid to relevant simulation models. In the present study, soil thermal conditions at a mountain meadow during the vegetation season were simulated. A dual-continuum model of coupled water and heat transport was employed to account for preferential flow effects. Data collected at an experimental site in the Sumava Mountains, southern Bohemia, during the vegetation season 2009 were employed. Soil hydraulic properties (retention curve and hydraulic conductivity) determined by independent soil tests were used. Unavailable hydraulic parameters were adjusted to obtain satisfactory hydraulic model performance. Soil thermal properties were estimated based on values found in literature without further optimization. Three different approaches were used to approximate the soil thermal conductivity function, lambda(theta): (i) relationships provided by Chung and Horton (ii) linear estimates as described by Loukili, Woodbury and Snelgrove, (iii) methodology proposed by Cote and Konrad. The simulated thermal conditions were compared to those observed. The impact of different soil thermal conductivity approximations on the heat transport simulation results was analysed. The differences between the simulation results in terms of the soil temperature were small. Regarding the surface soil heat flux, these differences became substantial. More realistic simulations were obtained using lambda(theta) estimates based on the soil texture and composition. The differences between these two, related to neglecting vs. considering lambda(theta) non-linearity, were found negligible.
  • Soil water and heat transport plays an important role in various hydrologic, agricultural, and industrial applications. Accordingly, an increasing attention is paid to relevant simulation models. In the present study, soil thermal conditions at a mountain meadow during the vegetation season were simulated. A dual-continuum model of coupled water and heat transport was employed to account for preferential flow effects. Data collected at an experimental site in the Sumava Mountains, southern Bohemia, during the vegetation season 2009 were employed. Soil hydraulic properties (retention curve and hydraulic conductivity) determined by independent soil tests were used. Unavailable hydraulic parameters were adjusted to obtain satisfactory hydraulic model performance. Soil thermal properties were estimated based on values found in literature without further optimization. Three different approaches were used to approximate the soil thermal conductivity function, lambda(theta): (i) relationships provided by Chung and Horton (ii) linear estimates as described by Loukili, Woodbury and Snelgrove, (iii) methodology proposed by Cote and Konrad. The simulated thermal conditions were compared to those observed. The impact of different soil thermal conductivity approximations on the heat transport simulation results was analysed. The differences between the simulation results in terms of the soil temperature were small. Regarding the surface soil heat flux, these differences became substantial. More realistic simulations were obtained using lambda(theta) estimates based on the soil texture and composition. The differences between these two, related to neglecting vs. considering lambda(theta) non-linearity, were found negligible. (en)
Title
  • On Parameterization of Heat Conduction in Coupled Soil Water and Heat Flow Modelling
  • On Parameterization of Heat Conduction in Coupled Soil Water and Heat Flow Modelling (en)
skos:prefLabel
  • On Parameterization of Heat Conduction in Coupled Soil Water and Heat Flow Modelling
  • On Parameterization of Heat Conduction in Coupled Soil Water and Heat Flow Modelling (en)
skos:notation
  • RIV/68407700:21110/12:00199025!RIV13-GA0-21110___
http://linked.open...avai/predkladatel
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA205/08/1174), Z(AV0Z20600510)
http://linked.open...iv/cisloPeriodika
  • 4
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
  • 156294
http://linked.open...ai/riv/idVysledku
  • RIV/68407700:21110/12:00199025
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • advective heat flux; dual-permeability model; preferential flow; soil heat transport; soil thermal conductivity; surface energy balance (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [DCF5A1D31C8B]
http://linked.open...i/riv/nazevZdroje
  • Soil and Water 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
  • 7
http://linked.open...iv/tvurceVysledku
  • Dohnal, Michal
  • Vogel, Tomáš
  • Votrubová, Jana
  • Tesař, M.
http://linked.open...ain/vavai/riv/wos
  • 000311588800001
http://linked.open...n/vavai/riv/zamer
issn
  • 1801-5395
number of pages
http://localhost/t...ganizacniJednotka
  • 21110
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