Zobrazeno 1 - 10
of 33
pro vyhledávání: '"Christian Fouillac"'
Publikováno v:
Aquatic Geochemistry. 7:81-105
The spatial and temporal distributions of major elements were investigated in the sur- face waters and in associated suspended matter at two sites of the upper Loire basin (Orleans and Brehemont) between 1995 and 1998. According to geochemical and is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::55e5f91855b178ce97ac1c7efce4de16
https://doi.org/10.1023/a:1017518831860
https://doi.org/10.1023/a:1017518831860
Publikováno v:
Chemical Geology. 170:179-201
The Loire River, with one of the largest watersheds in France, has been monitored just outside the city of Orleans since 1994. Physico-chemical parameters and major and trace elements were measured between 2-day and 1-week intervals according to the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aeef15c7b00f41412a122ce44196d1d1
https://doi.org/10.1016/s0009-2541(99)00247-8
https://doi.org/10.1016/s0009-2541(99)00247-8
Publikováno v:
Journal of Hydrology. 203:143-153
The French Massif Central has long been recognized as an area with numerous mineral water springs. It is often very difficult to measure the flow rate of mineral springs since they are spread out over extentive areas. Water from the Allier River has
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::51436202c227d42c75fb691e15aebb82
https://doi.org/10.1016/s0022-1694(97)00094-2
https://doi.org/10.1016/s0022-1694(97)00094-2
Publikováno v:
Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science. 325:119-124
Resume Dans cette note, nous presentons les variations spatiales des elements majeurs et traces et des isotopes (O, D, 87 Sr/ 86 Sr) de sources minerales selectionnees. La zone d'etude est le champ d'emergence des eaux minerales de la Limagne d'Allie
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bc968d289078becda881788d0872068e
https://doi.org/10.1016/s1251-8050(97)83972-9
https://doi.org/10.1016/s1251-8050(97)83972-9
Publikováno v:
Chemical Geology. 135:89-101
Surface and mineral waters from a geothermal area (Cezallier) in the centre of the Massif Central, France, were analysed for Sr isotopes, Sr and major elements in order to use Sr isotopes to investigate the discharge of a mineralised water area, espe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a49ade6fd8ff368733d705642ceafa5a
https://doi.org/10.1016/s0009-2541(96)00110-6
https://doi.org/10.1016/s0009-2541(96)00110-6
Autor:
Christian Fouillac, Mohamed Azaroual
Publikováno v:
Applied Geochemistry. 12:55-73
Distilled water was percolated for 38 days through Soultz granite (France) from the candidate site of the future Hot Dry Rock (HDR) geothermal exchanger at 180°C and 14 bars in a dynamic experimental system (plug-flow system with Ti reaction cell: I
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::57500b6b876faad6064a5d746d940c91
https://doi.org/10.1016/s0883-2927(96)00054-6
https://doi.org/10.1016/s0883-2927(96)00054-6
Autor:
Christian Fouillac
Publikováno v:
Integrated Science & Technology Program ISBN: 9789400766600
On a world-scale basis, fossil fuels are likely to remain the main sources for electricity generation in the twenty-first century, and many industrial processes that are also large CO2 emitters will still be active for many decades. Therefore, carbon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::92106b2c33cc4722483934aac4ed6236
https://doi.org/10.1007/978-94-007-6661-7_6
https://doi.org/10.1007/978-94-007-6661-7_6
Publikováno v:
Colloids and Surfaces A: Physicochemical and Engineering Aspects. 100:73-82
Li+ adsorption onto aluminium hydroxide has been investigated at various temperatures. Experiments were made on two high-salinity geothermal-type fluids in which the lithium concentration reaches values greater than 30 and 50 mmol −1 respectively,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fcb57a7f2fec3790ccf3e2523cf35ef8
https://doi.org/10.1016/0927-7757(95)03185-g
https://doi.org/10.1016/0927-7757(95)03185-g
Publikováno v:
Geochimica et Cosmochimica Acta. 57:2737-2749
Deep boreholes (⩽870 m) in the Upper Rhine Graben produce medium-temperature (120–150°C) saline fluids that circulate through the granitic basement and/or the overlying sedimentary rocks. The salinity of these deep fluids, sampled from both the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::02a721ede5c51ce8d51c550d121fee47
https://doi.org/10.1016/0016-7037(93)90387-c
https://doi.org/10.1016/0016-7037(93)90387-c
Publikováno v:
Applied Geochemistry. 7:243-255
Hydraulic injection-backflow tests were carried out in borehole GPK1 at a site designed for geothermal “Hot Dry Rock” experiments, located in the Rhine Graben near Soultz-sous-Foreˆts, France. The injected fresh water was in contact with granite
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e4e02445c9d0e582fbbf0b2837f0d312
https://doi.org/10.1016/0883-2927(92)90040-a
https://doi.org/10.1016/0883-2927(92)90040-a