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The layered double hydroxides (LDHs) of Mg with Ga and In decompose completely on heating to 500°C to yield poorly ordered oxide residues. In the Mg–Ga system, the oxide residue has a rock-salt structure with Ga incorporated in the MgO matrix. In the Mg–In system, the oxide residue is X-ray amorphous. These oxide residues revert back to the original LDH either on standing in a water-saturated atmosphere...
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