Rl. Penn et Jf. Banfield, Formation of rutile nuclei at anatase {112} twin interfaces and the phase transformation mechanism in nanocrystalline titania, AM MINERAL, 84(5-6), 1999, pp. 871-876
In nanocrystalline anatase coarsened under hydrothermal conditions (250 deg
rees C, P-sat), the anatase-to-rutile phase transformation is nucleated at
anatase {112} twin boundaries formed by oriented attachment. The anatase tw
in boundary is constructed from structural elements common to rutile. Speci
fically, rutile nucleation involves displacement of only one half the titan
ium cations within the twin slab. Subsequent transformation of bulk anatase
involves rupture of 7 of the 24 Ti-O bonds per unit cell and cooperative d
isplacement of Ti and O. As the transformation advances into the bulk mater
ial, adjacent slabs of anatase octahedra are destabilized, resulting in rap
id progression of the transformation of bulk anatase to rutile. The implied
chain reaction, scarcity of partly reacted crystals, absence of multiply t
winned rutile, and the importance of nucleation at anatase twins indicate a
rate law based on slow nucleation and rapid growth. The displacements are
comparable to those proposed previously for macroscopic anatase at much hig
her temperatures, indicating the atomic mechanism is not modified by partic
le size or temperature, despite the rapid kinetics in finely crystalline ag
gregates. In addition to the formation of twins, clusters with rutile-like
character may occur at some fraction of random anatase-anatase particle con
tacts. Such interfaces should result in decreased activation barriers for r
utile nucleation and, thus, contribute significantly to the observed faster
transformation rates in nanocrystalline compared to coarsely crystalline m
aterials.