The topotactic transformation of Ti3SiC2 into a partially ordered cubic Ti(C0.67Si0.06) phase by the diffusion of Si into molten cryolite

Immersion of Ti3SiC2 samples in molten cryolite at 960 degrees C resulted i n the preferential diffusion of Si atoms out of the basal planes to form a partially ordered, cubic phase with approximate chemistry Ti(C-0.67, Si-0.0 6) The latter forms in domains, wherein the (111) planes are related by mir ror planes; ie., the loss of Si results in the de-twinning of the Ti3C2 lay ers. Raman spectroscopy, X-ray diffraction, optical, scanning and transmiss ion electron microscopy all indicate that the Si exits the structure topota ctically, in such a way that the C atoms remain partially in their ordered position in the cubic phase. (C) 1999 The Electrochemical Society. S0013-46 51(98)12-106-7. All rights reserved.