The
detailed phase compositions in the NiMnCo–C system with
Mg2Si3O8·5H2O added
and its effects on {111} and {100} diamonds grown at 5.5 GPa and 1355
°C are reported. The results reveal that Mg2Si3O8·5H2O reacts with catalysts and
produces tephroite, forsterite, coesite, and H2O. With
its content in the carbon source increasing from 0.0 to 5.0 wt %,
the morphology of diamonds evolves from a bulky cubic octahedron/truncated
cube to a {111}/{100}skeleton with {110} dendrites and finally to
{100} antiskeletal dendrites. The concentration of nitrogen impurity
(N
total) in diamonds exhibits a N
total{111} > N
total{100} pattern and decreases from ∼117 and ∼100 to ∼36
and ∼21 ppm, respectively. Except liquid water inclusion, hydrogen
and oxygen are also found to enter the surfaces, grain boundaries,
inclusions, or cracks of the growing diamond in the form of −CH3, −CH2, and R1–CH(R2)–OH groups
and compete with nitrogen atoms entering the diamond lattice, thus
resulting in the decreased N
total. Besides,
the termination of diamond structure by C–H and C–OH
bonds is also controlled by the oriented density of step edge and
causes hydrocarbon group content C
{100} > C
{111} and crystal growth rate V
{100} > V
{111}.
The competition mechanism and the oriented density of step edge may
be used to constrain the formation environment and interpret the lower
nitrogen content in natural cubic and fibrous diamonds than in octahedral
diamonds.