Abstract
Two percolation experimental studies have been realized on Fontainebleau sand samples, taken in the zones where seasonal heat storage processes are foreseen. Evolutions of silica and potassium concentrations are evaluated. Water composition is examined with respect to reaction with various minerals (potassic feldspar, kaolinite, and an intermediate form between chalcedony and amorphous silica). A simulation is done with the STELE coupled model.
Citation Formats
Vinsot, A, and Mery, P.
Study of the geochemical effect of an underground thermal storage. The case of the Fontainebleau sands at St-Quentin-en-Yvelines.
France: N. p.,
1989.
Web.
Vinsot, A, & Mery, P.
Study of the geochemical effect of an underground thermal storage. The case of the Fontainebleau sands at St-Quentin-en-Yvelines.
France.
Vinsot, A, and Mery, P.
1989.
"Study of the geochemical effect of an underground thermal storage. The case of the Fontainebleau sands at St-Quentin-en-Yvelines."
France.
@misc{etde_10125495,
title = {Study of the geochemical effect of an underground thermal storage. The case of the Fontainebleau sands at St-Quentin-en-Yvelines}
author = {Vinsot, A, and Mery, P}
abstractNote = {Two percolation experimental studies have been realized on Fontainebleau sand samples, taken in the zones where seasonal heat storage processes are foreseen. Evolutions of silica and potassium concentrations are evaluated. Water composition is examined with respect to reaction with various minerals (potassic feldspar, kaolinite, and an intermediate form between chalcedony and amorphous silica). A simulation is done with the STELE coupled model.}
place = {France}
year = {1989}
month = {Dec}
}
title = {Study of the geochemical effect of an underground thermal storage. The case of the Fontainebleau sands at St-Quentin-en-Yvelines}
author = {Vinsot, A, and Mery, P}
abstractNote = {Two percolation experimental studies have been realized on Fontainebleau sand samples, taken in the zones where seasonal heat storage processes are foreseen. Evolutions of silica and potassium concentrations are evaluated. Water composition is examined with respect to reaction with various minerals (potassic feldspar, kaolinite, and an intermediate form between chalcedony and amorphous silica). A simulation is done with the STELE coupled model.}
place = {France}
year = {1989}
month = {Dec}
}