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Thermal analysis of synthetic reevesite and cobalt substituted reevesite (Ni,Co)6Fe2(OH)16(CO3) · 4H2O
Author(s) -
Kathleen H. Bakon,
Sara J. Palmer,
Ray L. Frost
Publication year - 2009
Publication title -
journal of thermal analysis and calorimetry
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.521
H-Index - 92
eISSN - 1588-2926
pISSN - 1388-6150
DOI - 10.1007/s10973-009-0145-x
Subject(s) - cobalt , thermal decomposition , brucite , carbonate , chemistry , decomposition , thermal stability , inorganic chemistry , dehydration , magnesium , organic chemistry , biochemistry
The mineral reevesite and the cobalt substituted reevesite have been synthesised. The d(003) spacings of the minerals ranged from 7.54 to 7.95 Å. The maximum d(003) value occurred at around Ni:Co 0.4:0.6. This maximum in interlayer distance is proposed to be due to a greater number of carbonate anions and water molecules intercalated into the structure. The stability of the reevesite and cobalt doped reevesite was determined by thermogravimetric analysis. The maximum temperature of the reevesite occurs for the unsubstituted reevesite and is around 220°C. The effect of cobalt substitution results in a decrease in thermal stability of the reevesites. Four thermal decomposition steps are observed and are attributed to dehydration, dehydroxylation and decarbonation, decomposition of the formed carbonate and oxygen loss at ~807 °C. A mechanism for the thermal decomposition of the reevesite and the cobalt substituted reevesite is proposed

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