Heating Fe oxide-rich soils increases the dissolution rate of metals

Clays and Clay Minerals

Volumn 54, Issue 2, 2006, Pages 165-175

  Perrier, Nicolas ^a,b,c   Gilkes, Robert J ^d   Colin, Fabrice ^a  

^a CEREGE   (France)

^b UNC   (New Caledonia)

^c Falconbrige   (New Caledonia)

^d UNIVERSITY OF WESTERN AUSTRALIA   (Australia)

Author keywords

Dehydroxylation acid dissolution; Goethite; Hematite; Lateritic ore; Maghemite; New Caledonia

Indexed keywords

CRYSTALS; DISSOLUTION; HEATING; IRON; OXIDES; SOILS; SOLUBILITY;

DEHYDROXYLATION ACID DISSOLUTION; GOETHITE; HEMATITE; LATERITIC ORE; MAGHEMITE;

METALS;

ALUMINUM; CHROMIUM; CRYSTAL STRUCTURE; DEHYDROXYLATION; DISSOLUTION; EXPERIMENTAL MINERALOGY; GOETHITE; HEATING; HEMATITE; MAGHEMITE; NICKEL; OXISOL;

KONIAMBO MASSIF; MELANESIA; NEW CALEDONIA [MELANESIA]; NEW CALEDONIA [NEW CALEDONIA (DPN)]; PACIFIC ISLANDS; PACIFIC OCEAN;

EID: 33646562888     PISSN: 00098604     EISSN: None     Source Type: Journal    
DOI: 10.1346/CCMN.2006.0540203     Document Type: Article

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