Solution controls for dissolved silica at 25, 50 and 90°C for quartz, Callovo-Oxfordian claystone, illite and MX80 bentonite

Physics and Chemistry of the Earth

Volumn 36, Issue 17-18, 2011, Pages 1648-1660

  Suzuki Muresan, Tomo ^a   Vandenborre, Johan ^a   Abdelouas, Abdesselam ^a   Grambow, Bernd ^a  

^a UNIVERSITÉ DE NANTES   (France)

Author keywords

Clay minerals; Dissolution; Precipitation rates; Silica; Solubility; Temperature

Indexed keywords

BATCH SYSTEMS; CHEMICAL COMPOSITIONS; CLAY MATERIALS; CLAYSTONES; CONTROLLED ATMOSPHERE; DISSOLUTION RATES; DISSOLVED SILICA; DYNAMIC PROCESS; ENGINEERED BARRIER SYSTEM; EXCHANGE REACTION; GEOLOGICAL FORMATION; HIGH LEVEL NUCLEAR WASTES; HOST ROCKS; ILLITE-SMECTITE; KEY ELEMENTS; LOW PERMEABILITY; MX-80 BENTONITE; NUCLEAR GLASS; NUCLEAR WASTE; PH VALUE; PORE WATERS; PRECIPITATION RATES; SILICIC ACIDS; SOLUBILITY VALUE;

BENTONITE; DISSOLUTION; EXPERIMENTS; GLASS; GROUNDWATER; LEACHING; QUARTZ; RADIOACTIVE TRACERS; RADIOACTIVE WASTE DISPOSAL; RADIOACTIVE WASTES; SILICA; SILICATES; SILICON; SOLUBILITY; TEMPERATURE; WASTE DISPOSAL;

CLAY MINERALS;

BENTONITE; CLAYSTONE; DISSOLUTION; DISSOLVED MATTER; ILLITE; MONTMORILLONITE; OXFORDIAN; PERMEABILITY; PRECIPITATION (CHEMISTRY); QUARTZ; RETENTION; SILICA; SMECTITE; SOLUBILITY; TEMPERATURE EFFECT;

EID: 82955247985     PISSN: 14747065     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.pce.2011.10.015     Document Type: Article

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