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  • The Benesov-Usti aquifer system of the Bohemian Cretaceous Basin constitutes the largest accumulation of moderately thermal groundwater (25 - 35oC) in the Czech Republic. The main goal of the research project was the determination of available yield of groundwater resources in the areas of Decin and Usti and effect of withdrawals on the quantity and temperature of the waters. The area is strongly influenced by Saxonian orogeny. Common approaches to the simulation of groundwater flow using MODFLOW packages BCF and LPF fails. Suitable simulation of the hydraulic function of faults and heat transfer simulations is only possible with discretization of the model layers independent of the location of the aquifers and aquitards. The MODFLOW using HUF package and MT3DMS model were evaluated as satisfied tools for the calculation of groundwater and heat flow. Potential for thermal groundwater abstraction up to 275 L.s-1 in Ústí city and 44 L.s-1in Děčín city accompanied by maximal drop of groundwater temperature 1.7oC were evaluated by predictive simulations.
  • The Benesov-Usti aquifer system of the Bohemian Cretaceous Basin constitutes the largest accumulation of moderately thermal groundwater (25 - 35oC) in the Czech Republic. The main goal of the research project was the determination of available yield of groundwater resources in the areas of Decin and Usti and effect of withdrawals on the quantity and temperature of the waters. The area is strongly influenced by Saxonian orogeny. Common approaches to the simulation of groundwater flow using MODFLOW packages BCF and LPF fails. Suitable simulation of the hydraulic function of faults and heat transfer simulations is only possible with discretization of the model layers independent of the location of the aquifers and aquitards. The MODFLOW using HUF package and MT3DMS model were evaluated as satisfied tools for the calculation of groundwater and heat flow. Potential for thermal groundwater abstraction up to 275 L.s-1 in Ústí city and 44 L.s-1in Děčín city accompanied by maximal drop of groundwater temperature 1.7oC were evaluated by predictive simulations. (en)
Title
  • Mathematical Modelling of the Groundwater and Heat Flow in the Complicated Hydrogeology Structures
  • Mathematical Modelling of the Groundwater and Heat Flow in the Complicated Hydrogeology Structures (en)
skos:prefLabel
  • Mathematical Modelling of the Groundwater and Heat Flow in the Complicated Hydrogeology Structures
  • Mathematical Modelling of the Groundwater and Heat Flow in the Complicated Hydrogeology Structures (en)
skos:notation
  • RIV/00216208:11310/13:10174166!RIV14-GA0-11310___
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA205/07/0691)
http://linked.open...iv/cisloPeriodika
  • 02
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
  • 86595
http://linked.open...ai/riv/idVysledku
  • RIV/00216208:11310/13:10174166
http://linked.open...riv/jazykVysledku
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  • Mathematical modelling; Heat Flow; Groundwater; Bohemian Cretaceous Basin (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • IN - Indická republika
http://linked.open...ontrolniKodProRIV
  • [E92E005535A4]
http://linked.open...i/riv/nazevZdroje
  • International Journal of Engineering Research and Technology
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
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http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 9
http://linked.open...iv/tvurceVysledku
  • Uhlík, J.
  • Baier, J.
  • Datel, Josef
issn
  • 2278-0181
number of pages
http://localhost/t...ganizacniJednotka
  • 11310
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