ADSORPTION OF AUCLZ BY KAOLINITES: EFFECT OF pH, TEMPERATURE AND KAOLINITE CRYSTALLINITY
Adsorption of the AuC1-4 complex by kaolinites of different crystallinities (Kao-1 and Kao-2) from 100 mL of AuC13-1-1C1.4H20 solutions containing 10,000, 500 and 50 mug/L Au and 1 g of kaolinite was measured at pH 3 to 9 at ambient temperature and 120 deg C. Adsorption from the 50, 500 and 10,000 l...
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Published in | Clays and clay minerals Vol. 51; no. 5; pp. 493 - 501 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
Published |
01.01.2003
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Online Access | Get full text |
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Summary: | Adsorption of the AuC1-4 complex by kaolinites of different crystallinities (Kao-1 and Kao-2) from 100 mL of AuC13-1-1C1.4H20 solutions containing 10,000, 500 and 50 mug/L Au and 1 g of kaolinite was measured at pH 3 to 9 at ambient temperature and 120 deg C. Adsorption from the 50, 500 and 10,000 lig Au/L solutions ranged from 64 to 100% at ambient temperature and from 68 to 100% at 120 deg C for both kaolinites. Adsorption was pH dependent with a maximum at pH < 5 and a minimum at neutral and alkaline pHs. Up to 1 mg Au/g kaolinite was adsorbed by the kaolinites at both ambient temperature and 120 deg C. In a separate Au adsorption experiment using 100 mL of 4000 mug Au/L solutions and 0.02 to 1.0 g of Kao-1, up to 8.55 mg Au/ g of kaolinite was adsorbed. The pH dependence of Au adsorption suggests that surface complexation of Au to alumina sites at the edges of kaolinite particles might be involved. Protonation of kaolinite surface sites might facilitate adsorption of the anionic Au complex. Both kaolinites adsorbed -100% of added Au at low pH values, but the less crystalline kaolinite (Kao-2) adsorbed more Au at high pH. Greater Au adsorption would be expected for the less crystalline Kao-2 sample if adsorption occurred at the edges of kaolinite particles. |
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Bibliography: | ObjectType-Article-2 SourceType-Scholarly Journals-1 content type line 23 ObjectType-Feature-1 |
ISSN: | 0009-8604 |
DOI: | 10.1346/CCMN.2003.0510503 |