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Volumn 58, Issue 2, 2010, Pages 280-291

Effects of temperature, pH, and iron/clay and liquid/clay ratios on experimental conversion of dioctahedral smectite to berthierine, chlorite, vermiculite, or saponite

Author keywords

Berthierine; Chlorite; Fe metal; Nuclear waste; Saponite; Smectite; Vermiculite

Indexed keywords

ALKALINE PH; BERTHIERINE; CHEMICAL TRANSFORMATIONS; CLAY FORMATION; CONCEPTUAL MODEL; CRITICAL PARAMETER; DEEP GEOLOGICAL REPOSITORY; DIOCTAHEDRAL SMECTITE; EFFECTS OF TEMPERATURE; EXPERIMENTAL CONVERSION; FE METAL; HIGH-LEVEL NUCLEAR WASTE REPOSITORY; HIGH-LEVEL NUCLEAR WASTES; HIGHER TEMPERATURES; LOW OXYGEN; LOW TEMPERATURES; MINERALOGICAL TRANSFORMATIONS; MORDENITES; NEAR-NEUTRAL PH; NEUTRAL PH; NUCLEAR WASTE; PALYGORSKITES; RICH PHASE; SMECTITES; STEEL CANISTERS;

EID: 77953299372     PISSN: 00098604     EISSN: None     Source Type: Journal    
DOI: 10.1346/CCMN.2010.0580212     Document Type: Article
Times cited : (66)

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