Rl. Penn et Jf. Banfield, ORIENTED ATTACHMENT AND GROWTH, TWINNING, POLYTYPISM, AND FORMATION OF METASTABLE PHASES - INSIGHTS FROM NANOCRYSTALLINE TIO2, The American mineralogist, 83(9-10), 1998, pp. 1077-1082
Atomic-resolution transmission electron micrographs show that nanocrys
talline TiO2 coarsens by oriented attachment and growth under hydrothe
rmal conditions. In addition to forming homogeneous single crystals, a
ttachment at anatase surfaces leads to twinning on {112} and intergrow
ths on (001) and {001}. Brookite, a polytype of anatase, occurs at som
e {112} twin surfaces. Alternating two octahedra-wide structural slabs
in brookite are shared with the two adjacent anatase twin domains. Be
cause {112} anatase twin interfaces contain one unit cell of brookite,
we propose that brookite may nucleate at twin planes and grow at the
expense of anatase. Alternatively, anatase-brookite interfaces may for
m by oriented attachment of primary brookite and anatase {112} crystal
lites. In this case, three unit cell-wide lamellae of brookite are int
erpreted as remnants of larger crystals that partly converted to anata
se by propagation of the anatase-brookite interface. Which phase is st
able is unclear over this particle size range, and products of random
thermal fluctuations may be preserved by quenching. Regardless of reac
tion direction, polytypic interconversion of anatase and brookite esse
ntially involves displacement of Ti (by c/4 brookite) into adjacent oc
tahedral sites in one of the pair of two octahedra-wide structural sla
bs. The results have broad relevance for nucleation and growth models
as they suggest that twinning and polytypism in macroscopic crystals c
an originate at oriented interfaces between primary nanocrystalline pa
rticles early in their crystallization history.