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The intercalation of cobalt ions (Co(II)) into the interlayer space of a layered silicate, magadiite, was conducted by ion exchange reactions between magadiite and aqueous solution of cobalt(II) chloride. Thermal treatment of the Co(II)-mgadiites in air at 1000°C resulted in the transformation to cristobalite with retaining the platy particle morphology of the original magadiite.
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Ogawa et al. (2007) studied this question.
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