H.O. Pierson. Handbook of carbon, graphite, diamond and fullerenes. Properties, processing and applications. 1993
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Carbon, |
Graphite, |
Diamond, |
and |
Fullerenes |
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In addition, |
electron |
diffraction |
patterns of polycrystalline |
diamond |
are |
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similar to those |
of basal-plane |
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oriented polycrystalline |
graphite |
and, |
when |
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analyzing |
mixtures |
of the two, |
it may be difficult |
to separate |
one pattern |
from |
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the |
other. |
Unfortunately, |
mixed |
graphite-carbon-diamond |
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aggregates |
are |
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common |
in natural |
and synthetic |
materials. |
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Raman |
Spectroscopy. |
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Fortunately |
an |
alternate |
solution |
to |
identifi- |
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cation is offered |
by Raman spectroscopy. |
This |
laser-optical |
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technique |
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can |
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determine |
with |
great’accuracy |
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the |
bonding |
states |
of the carbon |
atoms |
(sp* |
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for graphite |
or sp3 for diamond) |
by displaying |
theirvibrational |
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properties.t’) |
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The |
Raman |
spectra |
is the result |
of the |
inelastic scattering of optical |
photons |
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by lattice |
vibration |
phonons. |
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As |
shown |
in |
Fig. |
11.1, |
the |
presence |
of |
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diamond |
and/or |
graphite |
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bonding |
is unambiguous |
and clear. |
Single-crystal |
diamond |
is identified |
by |
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a single sharp |
Raman peak |
at 1332 |
cm (wave |
numbers), |
often |
referred to |
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as the D-band, |
and graphite |
by a broader |
peak |
near 1570 cm (the G-band) |
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and |
several |
second-order |
features. |
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500 |
1000 |
1500 |
2000 |
2500 |
3000 |
3500 |
Raman Shift (cm-l)
Figure 11.1. Raman spectra of diamond and graphite.
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Structure |
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and |
Properties |
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of Diamond |
247 |
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The |
Raman |
scattering |
efficiency |
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for sp2 bonds |
is more than |
fifty |
times |
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the efficiency |
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for |
sp3 bonds for |
graphitic |
domains |
smaller |
than |
10 nm. |
As |
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a result, |
the |
technique |
is capable |
of detecting |
minute |
amounts |
of graphite |
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bonds |
(such |
as may |
present |
in some |
diamond-like carbon). However, it |
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must |
be recognized |
that |
the |
techniques |
cannot |
readily |
define |
the |
state |
of |
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aggregation |
of the |
constituents. |
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Diamond |
Characteristics. |
It is generally |
accepted |
that, |
for a material |
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to be recognized |
as diamond, |
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it must |
have |
the |
following |
characteristics: |
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. A crystalline |
morphology |
visible |
by electron |
microscopy |
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. A single-phase |
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crystalline |
structure |
detectable |
by x-ray |
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or |
electron |
diffraction |
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. A clear |
diamond |
Raman spectrum |
with |
a sharp |
peak |
at |
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1332 cm |
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2.2 |
Atomic |
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Structure |
of Diamond |
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In Ch. 2, Sec. 3, the |
hybridization |
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of the |
carbon |
atom |
from the |
ground |
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state |
to the hybrid |
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sp3 (or tetragonal) |
orbital |
state |
is described. |
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It is shown |
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that |
this |
hybridization |
accounts |
for |
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the |
tetrahedral |
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symmetry |
and |
the |
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valence |
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state |
of four |
with |
four |
2sp3 |
orbitals found |
in |
the |
diamond |
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atomic |
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structure. |
These |
orbitals |
are |
bonded |
to |
the |
orbitals |
of four |
other |
carbon |
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atoms |
with a strong |
covalent |
bond |
(i.e., the |
atoms |
share |
a pair of electrons) |
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to form |
a regular tetrahedron |
with |
equal angles |
to each |
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other of 109” 28’, as |
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shown |
in Fig. |
11.2 |
(see |
also |
Fig. |
2.10 |
of Ch. |
2). |
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2.3Crystal Structures of Diamond
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Diamond is a relatively |
simple substance |
in the sense |
that |
its structure |
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and |
properties |
are |
essentially |
isotropic, |
in |
contrast |
to |
the pronounced |
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anisotropy |
of graphite. |
However, |
unlike |
graphite, |
it has |
several |
crystalline |
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forms and |
polytypes. |
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Cubic |
and Hexagonal |
Diamond. |
Each diamond |
tetrahedron |
com- |
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bines with four other tetrahedrato |
form strongly-bonded, |
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three-dimensional |
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and |
entirely |
covalent |
crystalline |
structures. |
Diamond |
has |
two |
such |
struc- |
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tures, one with |
a cubic |
symmetry |
(the more |
common |
and |
stable) and one |
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with |
a hexagonal |
symmetry |
found in nature as the |
mineral |
lonsdaleite |
(see |
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Sec. |
2.5). |
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248 Carbon, Graphite, Diamond, and Fullerenes
Figure 11.2.The diamond tetrahedron.
Structure |
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of |
Cubic |
Diamond. |
Cubic |
diamond |
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is |
by far |
the |
more |
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common |
structure and, in order to simplify the terminology, |
will |
be referred |
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to as simply “diamond”. |
The |
covalent |
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link |
between |
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the |
carbon |
atoms |
of |
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diamond |
is characterized |
by asmall |
bond |
length |
(0.154 |
nm) and a high bond |
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energy |
of 711 |
kJ/mol |
(170 kcal/mol).t*] |
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Each |
diamond |
unit cell |
has |
eight |
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atoms |
located |
as follows: |
l/8 |
x 8 at the |
corners, |
l/2 |
x 6 at the |
faces |
and |
4 |
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inside |
the |
unit |
cube. |
Two |
representations |
of the structure |
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are shown |
in Fig. |
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11.3, |
(a) and |
(b).t21t31 |
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The |
cubic |
structure |
of diamond |
can |
be visualized |
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as a stacking |
of |
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puckered |
infinite |
layers |
(the{1 |
11) planes) |
or as atwoface-centered |
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interpen- |
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etrating cubic lattices, one with |
origin |
at O,O,O,and the other |
at l/4,1/4,1/4, |
with |
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parallel axes, |
as shown |
in Fig. 11.3(c). |
The |
stacking |
sequence |
of the (111) |
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planes |
is ABCABC, |
so that every |
third |
layer |
is identical. |
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Density |
of |
Diamond. |
With its fourfold |
coordinated |
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tetrahedral |
(sp3) |
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bonds, |
the diamond |
structure |
is isotropic |
and, |
except |
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on the (111) |
plane, |
is |
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more |
compact |
than |
graphite |
(with |
its |
sp* |
anisotropic |
structure |
and |
wide |
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interlayer |
spacing). |
Consequently |
diamond |
has |
higher density |
than graph- |
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ite (3.515 |
g/cm3 |
vs. |
2.26 |
g/cm3). |
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Structure and Properties of Diamond 249
Sequence
Figure 11.3. Schematics of the structure of cubic diamond.[2][3]
Diamond has |
the |
highest |
atom density of any |
material |
with |
a molar |
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density |
of 0.293 g-atom/cm 3. |
As |
a result, |
diamond |
is the stiffest, |
hardest |
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and least compressible |
of all substances. |
In comparison, |
the |
molar |
density |
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of graphite is 0.188 |
g-atom/cm |
3. |
The atomic and crystal structure |
data of |
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diamond |
are summarized in Table |
11 .l .I41Also included |
in the table |
are the |
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data for |
hexagonal |
diamond (see |
Sec. 2.5). |
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250 Carbon, Graphite, Diamond, and Fullerenes
Table 11 .I. Crystal Structure Data of Diamond
Property
Space group
Atoms per unit cell
Atom position
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Cubic |
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Hexagonal |
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Symmetry |
Symmetry |
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Fd3m |
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PGJmmc |
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8 |
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4 |
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(000) |
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(000) |
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(i/2 |
- l/2 |
- 0) |
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(00 - 314) |
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(0 - |
l/2 |
- |
i/2) |
(l/8 |
- 213 - l/2) |
(l/2 |
- 0 - |
l/2) |
(l/8 |
- 213 - 718) |
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(l/4 |
- l/4 |
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- l/4) |
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(3/4 |
- 3/4 |
- l/4) |
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(l/4 |
- 3/4 |
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- 3/4) |
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(3/4 |
- l/4 |
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- 3/4) |
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Cell constant |
0.3567 |
a = 0.252 |
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at 298 K, nm |
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c = 0.142 |
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Theoretical |
density |
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at 298 K, g/cm3 |
3.5152 |
3.52 |
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Carbon-carbon |
bond |
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distance, |
nm |
0.15445 |
0.154 |
2.4Diamond Crystal Forms
Diamond |
occurs |
in several |
crystal forms |
(or habits) |
which |
include |
the |
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octahedron, |
the dodecahedron, |
and others |
which |
are more complicated. |
As |
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a reminder, |
the simple |
crystallographic |
planes |
(100,110 |
and |
111) in a cubic |
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crystal |
are |
shown |
in Fig. |
11 .4.t5j |
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These |
simple |
planes |
correspond |
to the faces ofthe |
three major |
crystal |
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forms |
of diamond: |
the |
(100) cubic, the (110) dodecahedral |
and |
the |
(111) |
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octahedral |
(Fig. 11.5). |
Both cubic |
and |
octahedral |
surfaces |
predominate |
in |
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high-pressure |
synthetic diamond |
where |
they |
are found |
alone |
or in combi- |
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nation |
to form |
blocky |
crystals.t6j |
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In CVD diamond, |
the (111) |
octahedral |
and |
the (100) |
cubic |
surfaces |
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predominate |
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and |
cube-octahedral |
crystals |
combining |
both of these |
sur- |
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faces |
are |
commonly |
found. |
Twinning |
occurs |
frequently |
on |
the |
(111) |
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surface. Faceted |
crystals |
of cut diamonds |
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are predominantly |
the |
(111) |
and |
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(100) |
surfaces. |
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Structure and Properties of Diamond 251
(100) Plane |
(110) Plane |
C
b ‘_“..” .. 0
@
(111) Plan:
Figure 11.4. Indices of some simple planes in a cubic crystal.[q
Cubic {loo} |
Dodecahedron (110) |
z
t Y
i
v’, X
Octahedron {ill}
Figure 11.5. Major crystal forms of diamond.
252 Carbon, Graphite, Diamond, and Fullerenes
Diamond Cleavage Planes. Diamond breaks along well-defined
cleavage |
planes |
(the cleavage |
of a crystal being |
its characteristic |
of |
breaking along given crystallographic planes where |
the yield strength |
is |
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lower due to a high concentration |
of weaker bonds or a lower total number |
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of bonds). The dominant cleavage plane is the (111) |
but many others have |
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been observed. |
This cleavage |
characteristic is the |
key to the cutting of |
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gemstones |
(see Ch. 12). The cleavage energies of the various planes are |
reviewed in Sec. 6.0.
2.5The Polytypes of Diamond
Hexagonal Diamond. Hexagonal diamond is an allotropic form of carbon which is close to cubic diamond in structure and properties. It is a polytype of diamond, that is a special form of polymorph where the closepacked layers ((111) for cubic and (100) for hexagonal) are identical but have a different stacking sequence. Hexagonal diamond has an ABAB stacking sequence, so that every second layer is identical as shown in Fig. 11.6.m This two-layer hexagonal sequence (known as 2H diamond) is different in this respect from the three-layer sequence of cubic diamond (known as 3C diamond). The crystallographic data of these two polytypes are listed in Table 11 .I .
A-
B-
C-
Note ABAB Sequence
Figure 11.6. Schematic of the structure of hexagonal diamond (lonsdaleite).~~
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Structure |
and |
Properties |
of Diamond |
253 |
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The cubic diamond |
nucleus |
is slightly |
more stable than the hexagonal |
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with an energy |
difference |
between |
the |
two |
of only 0.1 - 0.2 eV per carbon |
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atom. |
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Because of this |
small |
energy |
difference, |
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the |
growth |
mechanism |
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leading |
to the |
hexagonal |
structure |
instead |
of cubic can readily occur. The |
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inclusion |
of hexagonal |
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diamond |
in a cubic |
diamond |
structure |
is equivalent |
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to |
having |
a |
stacking |
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fault |
at |
every |
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two-atom |
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layer |
and |
is |
generally |
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detrimental |
to |
optical |
and |
other |
properties. |
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Hexagonal |
Diamond |
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Occurrence. |
The |
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formation |
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of hexagonal |
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diamond |
is usually favored where |
high |
carbon |
supersaturation |
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is prevalent, |
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a condition |
commonly found during |
CVD |
synthesis |
and |
occasionally |
during |
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high-pressure |
synthesi@lt9) |
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(see Ch. 12). Natural |
diamond |
grows at much |
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lower |
supersaturation |
levels |
and consequently |
natural |
hexagonal |
diamond |
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is rarely |
found.tlO) |
The |
natural |
hexagonal |
diamond |
is known |
as the mineral |
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lonsdaleite. |
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Some meteoriies |
contain |
diamond |
such |
as the |
one |
found |
in Canyon |
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Diablo in Arizona. |
The |
diamond |
is in the form |
of polycrystalline |
compacts |
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made |
up of submicron |
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crystals. |
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These |
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crystals |
are |
mostly |
cubic |
although |
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the |
hexagonal |
form is also |
found. |
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6H |
Diamond. |
Recent |
investigations |
have |
revealed |
the existence |
of |
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another |
intermediate |
diamond |
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polytype |
known |
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as |
6H |
diamond.t5) |
This |
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material |
is believed |
to belong |
to a hypothetical |
series |
of diamond |
typeswith |
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structures |
intermediate |
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between |
hexagonal |
and cubic. |
The membersofthis |
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series |
are |
tentatively |
identified |
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as |
4H, |
6H, 8H, |
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10H. |
The |
series |
would |
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include |
hexagonal |
(2H) diamond |
on one end and cubic |
(3C) diamond |
on the |
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other |
(the digit |
indicates |
the number |
of layers). |
The existence |
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of 4H, 8H and |
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1OH diamonds |
has yet to be confirmed. |
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The |
6H |
structure |
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has |
a |
mixed |
six-layer |
hexagonal/cubic |
stacking |
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sequence |
AA’C’B’BC, |
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shown |
schematically |
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in Fig.1 1.7.p) |
It may exist |
in |
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CVD |
diamond. |
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3.0 IMPURITIES IN DIAMOND AND CLASSIFICATION
3.1Impurities
The properties of diamond |
are susceptible |
to impurities and the presence |
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of even |
a minute |
amount of a foreign element |
such |
as nitrogen can |
cause |
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drastic |
changes. |
It is therefore |
important to |
know |
the composition |
of the |
254 Carbon, Graphite, Diamond, and Fullerenes
A
B
C
A’
B’
C’
A
Hexagonal Stacking: A-A’, B-B’
Cubic Stacking: Other adjacent Layers
Figure 11.7. Schematic of the structure of 6H diamond.f5]
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Structure |
and Properties |
of Diamond |
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255 |
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material |
being tested |
as |
accurately |
as possible |
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in order |
to obtain |
a true |
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evaluation |
of the |
measured |
properties. |
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Types of Impurities. |
Diamond, |
synthetic |
or natural, |
is never completely |
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free of impurities. |
These |
impurities |
are |
divided into two |
different |
types: |
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1. |
Lattice |
impurities |
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which |
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consist |
of |
foreign |
elements |
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incorporated |
in the |
lattice, |
the |
foreign |
atom replacing |
a |
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carbon |
atom. |
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2. |
Inclusions, |
which |
are |
separate |
particles |
and |
not |
part |
of |
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the |
lattice, |
usually |
consist |
of |
silicates |
of |
aluminum, |
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magnesium, |
or calcium |
such |
as olivine.f”j |
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The two major lattice impurities |
found |
in diamond |
are nitrogen |
and |
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boron. |
These |
two elements |
are the neighbors |
of carbon in the periodic |
table. |
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They |
have small |
atomic |
radii |
and |
fit |
readily |
within |
the |
diamond |
structure. |
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Other |
elemental |
impurities |
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may also |
be present |
but only |
in extremely |
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small |
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amounts |
and |
their effect |
on the |
properties |
of the |
material |
is still |
uncertain |
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but |
probably |
minor.t12] |
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Nitrogen. |
Nitrogen |
impurity |
in diamond |
is detected |
and characterized |
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by |
IR absorption |
and |
paramagnetic |
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resonance. |
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The majority of nitrogen |
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atoms |
within |
the |
diamond |
structure |
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are |
arranged |
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in pairs as shown |
in Fig. |
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11.8.[“] Isolated nitrogen atoms are |
rarer. |
Nitrogen |
platelets |
are |
also |
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present and can be represented |
as a quasi-planar |
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structure |
within the cube |
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(100) |
plane of the diamond |
crystal. |
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Their |
exact |
form is still controversial. |
Carbon atom
Nitrogen atom
8%
Figure 11.8. Schematic of a nitrogen pair impurity in the lattice structure of diamond.Lg]