Fayalite dissolution and siderite formation in water-saturated supercritical CO 2

Chemical Geology

Volumn 332-333, Issue , 2012, Pages 124-135

  Qafoku, Odeta ^a   Kovarik, Libor ^a   Kukkadapu, Ravi K ^a   Ilton, Eugene S ^a   Arey, Bruce W ^a   Tucek, Jiri ^b   Felmy, Andrew R ^a  

^a PACIFIC NORTHWEST NATIONAL LABORATORY   (United States)

^b PALACKÝ UNIVERSITY   (Czech Republic)

Author keywords

Fayalite dissolution; Olivines; Siderite; Supercritical CO 2; Water saturated

Indexed keywords

ANOXIC CONDITIONS; BASALTIC ROCKS; FAYALITE; HIGH PRESSURE; HIGH TEMPERATURE; HIGH-RESOLUTION TEM; HOST ROCKS; LIQUID WATER; MINERAL CARBONATES; RHOMBOHEDRAL MORPHOLOGY; SIDERITE; SSBAUER SPECTROSCOPIES; SUPERCRITICAL CO; SUPERCRITICAL-CO 2; SURFACE CHARACTERIZATION; VERTICAL STRUCTURES; WATER-SATURATED;

BATCH REACTORS; CARBONATION; DISSOLUTION; EXPERIMENTS; HIGH RESOLUTION TRANSMISSION ELECTRON MICROSCOPY; IRON ORES; LIQUIDS; OLIVINE; SCANNING ELECTRON MICROSCOPY; X RAY DIFFRACTION;

CARBON DIOXIDE;

CARBON DIOXIDE; DISSOLUTION; FAYALITE; GEOMORPHOLOGY; HOST ROCK; IMMOBILIZATION; OLIVINE; SIDERITE;

EID: 84867610358     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2012.09.028     Document Type: Article

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