No.269 Geodynamics Seminar
"Synthesis of "amorphous" diamond from graphite under static
high pressure and high temperature"
Dr. Hiroaki Ohfuji (Assistant Professor, GRC)
4:30 pm 〜, 16 July 2010
Meeting room "Glova", 4 floor, Integrated Research
Building
Abstract
Amorphous diamond is a unique carbon material which is characterized by
x-ray and electron diffractometry as amorphous in the long-range order
and by electron energy loss spectroscopy as diamond in the short-range
order. It was first synthesized from C60 fullerene by shock compression
and rapid-quenching techniques (Hirai et al., 1991) and also recently
obtained from neutron-radiated graphite, which involves a large number
of lattice defects, by similar experimental techniques (Niwase et al.,
2009). The key for the successful synthesis of amorphous diamond seems
to be, 1) the presence of modified sp2-bonded carbon in the starting
material to induce simultaneous and homogeneous nucleation of diamond
and 2) extremely rapid quenching from high temperature to minimize the
grain growth of individual nuclei.
In the present study, we conducted a series of laser-heated diamond anvil
cell (LHDAC) experiments using three types of low-crystalline carbon materials
(finely-milled graphite, glassy carbon and amorphous carbon) to test whether
amorphous diamond can be obtained also by static high pressure experiments.
The results suggest that low-crystalline carbon materials which involve
a considerable amount of modified sp2 (sp3-like) bondings and relatively
low heating temperature (ca. 1500 K) are essential for successful synthesis
of amorphous diamond under static high pressure (~25 GPa). The former provides
preferential nucleation sites for diamond, resulting in explosive spontaneous
nucleation and the latter plays a role in suppressing the subsequent grain
growth to freeze the unique amorphous characteristics.
For inquiry:Taku Tsuchiya TEL:(089)927-8198
E-mail takut@sci.ehime-u.ac.jp
