The thermal decomposition of basic aluminium oxalate has been studied by thermogravimetric and X-ray powder diffraction methods. It is suggested that the decomposition is similar to that of gibbsite, and that the original structure is a three-dimensional array of aluminium, oxalate, and hydroxyl ions in a distorted gibbsite lattice.
D. Dollimore, J. Dollimore and P. D. Perry, J. Chem. Soc. A, 1967, 448 DOI: 10.1039/J19670000448
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