Forward dissolution rate of silicate glasses of nuclear interest in clay-equilibrated groundwater

Chemical Geology

Volumn 330-331, Issue , 2012, Pages 207-217

  Jollivet, P ^a   Gin, S ^a   Schumacher, S ^b  

^a DIF   (France)

^b ANDRA   (France)

Author keywords

Alkali metal cations; Alkaline earth cations; Dissolution; Forward rate; Glasses; Ionic strength of solution

Indexed keywords

ALKALI METAL CATIONS; ALKALINE EARTH; ALKALINE EARTH CATIONS; APPARENT ACTIVATION ENERGY; CALCIUM IONS; DISSOLUTION RATES; FORWARD RATE; GLASS DISSOLUTION; METAL SITES; MOLE FRACTION; RATE INCREASE; SILICATE GLASS; SODIUM IONS; SON68 GLASS; SPECIFIC EFFECTS;

ALKALINE EARTH METALS; ALUMINUM; BOROSILICATE GLASS; CESIUM; CESIUM COMPOUNDS; DEIONIZED WATER; GLASS; GROUNDWATER; IONIC STRENGTH; METAL IONS; OXYGEN; POSITIVE IONS; SILICATES; ZIRCONIUM;

DISSOLUTION;

ALKALINE EARTH METAL; ANION; BORON; CATION; DISSOLUTION; GROUNDWATER; HYDROLYSIS; OXYGEN; REACTION KINETICS; SILICATE; SILICON;

EID: 84866660602     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.chemgeo.2012.09.012     Document Type: Article

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