An oxy-acetylene flame, impinging vertically upward on an Si(001) subs
trate, is systematically examined for morphological variations in the
resulting diamond deposits. The flame is operated under near neutral (
O2/CH2 ratio near 1.0) conditions in the unconfined, open atmosphere.
Singly twinned crystal morphologies in addition to the usual (001) fac
eted structures are observed and reported for the first time. Similar
morphological variations are observed along the radial as well as the
axial (vertical) coordinate directions in the flame. Large changes in
morphology are observed for changes in vertical position as small as 5
0 mum.