A thermodynamic model for the prediction of pore water composition of clayey rock at 25 and 80°C - Comparison with results from hydrothermal alteration experiments

Chemical Geology

Volumn 334, Issue , 2012, Pages 62-76

  Beaucaire, C ^a   Tertre, E ^b   Ferrage, E ^b   Grenut, B ^a   Pronier, S ^b   Made B ^c  

^a DIF   (France)

^b UNIVERSITÉ DE POITIERS   (France)

^c ANDRA   (France)

Author keywords

Clayey pore water chemistry; Hydrothermal alteration experiments; Thermodynamic model at 25 and 80 C; X ray diffraction profile modeling

Indexed keywords

EXPERIMENTAL MINERALOGY; FORECASTING; HIGH RESOLUTION TRANSMISSION ELECTRON MICROSCOPY; HYDROCHEMISTRY; KAOLINITE; ROCKS; TEMPERATURE DISTRIBUTION; WATER; X RAY DIFFRACTION;

CALLOVO-OXFORDIAN CLAYS; CHEMICAL COMPOSITIONS; DISSOLUTION PRECIPITATIONS; HYDROTHERMAL ALTERATIONS; PORE-WATER CHEMISTRY; TEMPERATURE DEPENDENCE; THERMODYNAMIC MODEL; X RAY DIFFRACTION PROFILE;

CLAY ALTERATION;

CALCITE; CHLORITE; DOLOMITE; EXPERIMENTAL MINERALOGY; EXPERIMENTAL STUDY; HYDROTHERMAL ALTERATION; ILLITE; KAOLINITE; MODEL TEST; MODEL VALIDATION; MONTMORILLONITE; NUMERICAL MODEL; P-T CONDITIONS; POREWATER; PREDICTION; QUARTZ; THERMODYNAMICS; X-RAY DIFFRACTION;

EID: 84868233090     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2012.09.040     Document Type: Article

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