Abstract
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.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have