Abstract
A quasi 3D hydrodynamical model of the Dogger aquifer in the Paris area has been established through a finite difference scheme. The model has appeared able to describe some real charateristics of the Dogger (piezometry, transmittivity, salt, helium and Carbon 14 distributions). A discordance between Darcy speeds derived from the hydrodynamical model (0.15 m/y) and localized dilution findings (15-17 m/y) is shown. It could be explained by an interference phenomenon in the measuring wells or a flow-thermal transfer-salt transfer coupling phenomenon that had not been taken into account in the model. Results indicate that the first hypothesis should be the good one.
Citation Formats
Wei, H F, and Ledoux, E.
A joint modelization of flow, temperature and salinity in the Dogger geothermal aquifer.
France: N. p.,
1990.
Web.
Wei, H F, & Ledoux, E.
A joint modelization of flow, temperature and salinity in the Dogger geothermal aquifer.
France.
Wei, H F, and Ledoux, E.
1990.
"A joint modelization of flow, temperature and salinity in the Dogger geothermal aquifer."
France.
@misc{etde_10117786,
title = {A joint modelization of flow, temperature and salinity in the Dogger geothermal aquifer}
author = {Wei, H F, and Ledoux, E}
abstractNote = {A quasi 3D hydrodynamical model of the Dogger aquifer in the Paris area has been established through a finite difference scheme. The model has appeared able to describe some real charateristics of the Dogger (piezometry, transmittivity, salt, helium and Carbon 14 distributions). A discordance between Darcy speeds derived from the hydrodynamical model (0.15 m/y) and localized dilution findings (15-17 m/y) is shown. It could be explained by an interference phenomenon in the measuring wells or a flow-thermal transfer-salt transfer coupling phenomenon that had not been taken into account in the model. Results indicate that the first hypothesis should be the good one.}
place = {France}
year = {1990}
month = {Dec}
}
title = {A joint modelization of flow, temperature and salinity in the Dogger geothermal aquifer}
author = {Wei, H F, and Ledoux, E}
abstractNote = {A quasi 3D hydrodynamical model of the Dogger aquifer in the Paris area has been established through a finite difference scheme. The model has appeared able to describe some real charateristics of the Dogger (piezometry, transmittivity, salt, helium and Carbon 14 distributions). A discordance between Darcy speeds derived from the hydrodynamical model (0.15 m/y) and localized dilution findings (15-17 m/y) is shown. It could be explained by an interference phenomenon in the measuring wells or a flow-thermal transfer-salt transfer coupling phenomenon that had not been taken into account in the model. Results indicate that the first hypothesis should be the good one.}
place = {France}
year = {1990}
month = {Dec}
}