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H.O. Pierson. Handbook of carbon, graphite, diamond and fullerenes. Properties, processing and applications. 1993

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246

Carbon,

Graphite,

Diamond,

and

Fullerenes

 

 

 

 

 

 

 

 

In addition,

electron

diffraction

patterns of polycrystalline

diamond

are

similar to those

of basal-plane

 

oriented polycrystalline

graphite

and,

when

analyzing

mixtures

of the two,

it may be difficult

to separate

one pattern

from

the

other.

Unfortunately,

mixed

graphite-carbon-diamond

 

aggregates

are

common

in natural

and synthetic

materials.

 

 

 

 

 

 

 

 

 

 

 

Raman

Spectroscopy.

 

Fortunately

an

alternate

solution

to

identifi-

cation is offered

by Raman spectroscopy.

This

laser-optical

 

technique

 

can

determine

with

great’accuracy

 

the

bonding

states

of the carbon

atoms

(sp*

for graphite

or sp3 for diamond)

by displaying

theirvibrational

 

properties.t’)

The

Raman

spectra

is the result

of the

inelastic scattering of optical

photons

by lattice

vibration

phonons.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

As

shown

in

Fig.

11.1,

the

presence

of

 

diamond

and/or

graphite

bonding

is unambiguous

and clear.

Single-crystal

diamond

is identified

by

a single sharp

Raman peak

at 1332

cm (wave

numbers),

often

referred to

as the D-band,

and graphite

by a broader

peak

near 1570 cm (the G-band)

and

several

second-order

features.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

I

I

 

 

I

 

I

 

 

I

 

I

 

 

I

 

 

 

 

 

8

-

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

500

1000

1500

2000

2500

3000

3500

Raman Shift (cm-l)

Figure 11.1. Raman spectra of diamond and graphite.

 

 

 

 

 

 

 

 

 

 

Structure

 

and

Properties

 

of Diamond

247

 

The

Raman

scattering

efficiency

 

for sp2 bonds

is more than

fifty

times

the efficiency

 

for

sp3 bonds for

graphitic

domains

smaller

than

10 nm.

As

a result,

the

technique

is capable

of detecting

minute

amounts

of graphite

bonds

(such

as may

present

in some

diamond-like carbon). However, it

must

be recognized

that

the

techniques

cannot

readily

define

the

state

of

aggregation

of the

constituents.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Diamond

Characteristics.

It is generally

accepted

that,

for a material

to be recognized

as diamond,

 

it must

have

the

following

characteristics:

 

 

 

. A crystalline

morphology

visible

by electron

microscopy

 

 

 

 

 

 

. A single-phase

 

crystalline

structure

detectable

by x-ray

 

 

 

 

 

 

or

electron

diffraction

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

. A clear

diamond

Raman spectrum

with

a sharp

peak

at

 

 

 

 

 

 

1332 cm

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

2.2

Atomic

 

Structure

of Diamond

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

In Ch. 2, Sec. 3, the

hybridization

 

of the

carbon

atom

from the

ground

state

to the hybrid

 

sp3 (or tetragonal)

orbital

state

is described.

 

It is shown

that

this

hybridization

accounts

for

 

the

tetrahedral

 

symmetry

and

the

valence

 

state

of four

with

four

2sp3

orbitals found

in

the

diamond

 

atomic

structure.

These

orbitals

are

bonded

to

the

orbitals

of four

other

carbon

atoms

with a strong

covalent

bond

(i.e., the

atoms

share

a pair of electrons)

to form

a regular tetrahedron

with

equal angles

to each

 

other of 109” 28’, as

shown

in Fig.

11.2

(see

also

Fig.

2.10

of Ch.

2).

 

 

 

 

 

 

 

 

 

 

2.3Crystal Structures of Diamond

 

Diamond is a relatively

simple substance

in the sense

that

its structure

and

properties

are

essentially

isotropic,

in

contrast

to

the pronounced

anisotropy

of graphite.

However,

unlike

graphite,

it has

several

crystalline

forms and

polytypes.

 

 

 

 

 

 

 

 

 

 

 

 

 

Cubic

and Hexagonal

Diamond.

Each diamond

tetrahedron

com-

bines with four other tetrahedrato

form strongly-bonded,

 

three-dimensional

and

entirely

covalent

crystalline

structures.

Diamond

has

two

such

struc-

tures, one with

a cubic

symmetry

(the more

common

and

stable) and one

with

a hexagonal

symmetry

found in nature as the

mineral

lonsdaleite

(see

Sec.

2.5).

 

 

 

 

 

 

 

 

 

 

 

 

 

 

248 Carbon, Graphite, Diamond, and Fullerenes

Figure 11.2.The diamond tetrahedron.

Structure

 

of

Cubic

Diamond.

Cubic

diamond

 

is

by far

the

more

common

structure and, in order to simplify the terminology,

will

be referred

to as simply “diamond”.

The

covalent

 

link

between

 

the

carbon

atoms

of

diamond

is characterized

by asmall

bond

length

(0.154

nm) and a high bond

energy

of 711

kJ/mol

(170 kcal/mol).t*]

 

Each

diamond

unit cell

has

eight

atoms

located

as follows:

l/8

x 8 at the

corners,

l/2

x 6 at the

faces

and

4

inside

the

unit

cube.

Two

representations

of the structure

 

are shown

in Fig.

11.3,

(a) and

(b).t21t31

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

The

cubic

structure

of diamond

can

be visualized

 

as a stacking

of

puckered

infinite

layers

(the{1

11) planes)

or as atwoface-centered

 

interpen-

etrating cubic lattices, one with

origin

at O,O,O,and the other

at l/4,1/4,1/4,

with

parallel axes,

as shown

in Fig. 11.3(c).

The

stacking

sequence

of the (111)

planes

is ABCABC,

so that every

third

layer

is identical.

 

 

 

 

 

 

Density

of

Diamond.

With its fourfold

coordinated

 

tetrahedral

(sp3)

bonds,

the diamond

structure

is isotropic

and,

except

 

on the (111)

plane,

is

more

compact

than

graphite

(with

its

sp*

anisotropic

structure

and

wide

interlayer

spacing).

Consequently

diamond

has

higher density

than graph-

ite (3.515

g/cm3

vs.

2.26

g/cm3).

 

 

 

 

 

 

 

 

 

 

 

 

 

 

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

density

of 0.293 g-atom/cm 3.

As

a result,

diamond

is the stiffest,

hardest

and least compressible

of all substances.

In comparison,

the

molar

density

of graphite is 0.188

g-atom/cm

3.

The atomic and crystal structure

data of

diamond

are summarized in Table

11 .l .I41Also included

in the table

are the

data for

hexagonal

diamond (see

Sec. 2.5).

 

 

 

 

250 Carbon, Graphite, Diamond, and Fullerenes

Table 11 .I. Crystal Structure Data of Diamond

Property

Space group

Atoms per unit cell

Atom position

 

Cubic

 

Hexagonal

Symmetry

Symmetry

 

Fd3m

 

 

PGJmmc

 

8

 

 

 

4

 

(000)

 

 

(000)

(i/2

- l/2

- 0)

 

(00 - 314)

(0 -

l/2

-

i/2)

(l/8

- 213 - l/2)

(l/2

- 0 -

l/2)

(l/8

- 213 - 718)

(l/4

- l/4

 

- l/4)

 

 

(3/4

- 3/4

- l/4)

 

 

(l/4

- 3/4

 

- 3/4)

 

 

(3/4

- l/4

 

- 3/4)

 

 

Cell constant

0.3567

a = 0.252

at 298 K, nm

 

c = 0.142

Theoretical

density

 

at 298 K, g/cm3

3.5152

3.52

Carbon-carbon

bond

 

distance,

nm

0.15445

0.154

2.4Diamond Crystal Forms

Diamond

occurs

in several

crystal forms

(or habits)

which

include

the

octahedron,

the dodecahedron,

and others

which

are more complicated.

As

a reminder,

the simple

crystallographic

planes

(100,110

and

111) in a cubic

crystal

are

shown

in Fig.

11 .4.t5j

 

 

 

 

 

 

 

 

 

 

 

 

These

simple

planes

correspond

to the faces ofthe

three major

crystal

forms

of diamond:

the

(100) cubic, the (110) dodecahedral

and

the

(111)

octahedral

(Fig. 11.5).

Both cubic

and

octahedral

surfaces

predominate

in

high-pressure

synthetic diamond

where

they

are found

alone

or in combi-

nation

to form

blocky

crystals.t6j

 

 

 

 

 

 

 

 

 

 

 

 

In CVD diamond,

the (111)

octahedral

and

the (100)

cubic

surfaces

predominate

 

and

cube-octahedral

crystals

combining

both of these

sur-

faces

are

commonly

found.

Twinning

occurs

frequently

on

the

(111)

surface. Faceted

crystals

of cut diamonds

 

are predominantly

the

(111)

and

(100)

surfaces.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

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

lower due to a high concentration

of weaker bonds or a lower total number

of bonds). The dominant cleavage plane is the (111)

but many others have

been observed.

This cleavage

characteristic is the

key to the cutting of

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).~~

 

 

 

 

 

 

 

 

 

 

Structure

and

Properties

of Diamond

253

 

 

The cubic diamond

nucleus

is slightly

more stable than the hexagonal

with an energy

difference

between

the

two

of only 0.1 - 0.2 eV per carbon

atom.

 

Because of this

small

energy

difference,

 

the

growth

mechanism

leading

to the

hexagonal

structure

instead

of cubic can readily occur. The

inclusion

of hexagonal

 

diamond

in a cubic

diamond

structure

is equivalent

to

having

a

stacking

 

fault

at

every

 

two-atom

 

layer

and

is

generally

detrimental

to

optical

and

other

properties.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Hexagonal

Diamond

 

Occurrence.

The

 

formation

 

of hexagonal

diamond

is usually favored where

high

carbon

supersaturation

 

is prevalent,

a condition

commonly found during

CVD

synthesis

and

occasionally

during

high-pressure

synthesi@lt9)

 

(see Ch. 12). Natural

diamond

grows at much

lower

supersaturation

levels

and consequently

natural

hexagonal

diamond

is rarely

found.tlO)

The

natural

hexagonal

diamond

is known

as the mineral

lonsdaleite.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Some meteoriies

contain

diamond

such

as the

one

found

in Canyon

Diablo in Arizona.

The

diamond

is in the form

of polycrystalline

compacts

made

up of submicron

 

crystals.

 

These

 

crystals

are

mostly

cubic

although

the

hexagonal

form is also

found.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

6H

Diamond.

Recent

investigations

have

revealed

the existence

of

another

intermediate

diamond

 

polytype

known

 

as

6H

diamond.t5)

This

material

is believed

to belong

to a hypothetical

series

of diamond

typeswith

 

structures

intermediate

 

between

hexagonal

and cubic.

The membersofthis

 

series

are

tentatively

identified

 

as

4H,

6H, 8H,

 

10H.

The

series

would

include

hexagonal

(2H) diamond

on one end and cubic

(3C) diamond

on the

other

(the digit

indicates

the number

of layers).

The existence

 

of 4H, 8H and

1OH diamonds

has yet to be confirmed.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

The

6H

structure

 

has

a

mixed

six-layer

hexagonal/cubic

stacking

sequence

AA’C’B’BC,

 

shown

schematically

 

in Fig.1 1.7.p)

It may exist

in

CVD

diamond.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

3.0 IMPURITIES IN DIAMOND AND CLASSIFICATION

3.1Impurities

The properties of diamond

are susceptible

to impurities and the presence

of even

a minute

amount of a foreign element

such

as nitrogen can

cause

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]

 

 

 

 

 

 

 

 

Structure

and Properties

of Diamond

 

255

material

being tested

as

accurately

as possible

 

in order

to obtain

a true

evaluation

of the

measured

properties.

 

 

 

 

 

 

 

 

 

 

 

Types of Impurities.

Diamond,

synthetic

or natural,

is never completely

free of impurities.

These

impurities

are

divided into two

different

types:

 

 

1.

Lattice

impurities

 

which

 

consist

of

foreign

elements

 

 

 

 

 

incorporated

in the

lattice,

the

foreign

atom replacing

a

 

 

 

 

 

carbon

atom.

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

2.

Inclusions,

which

are

separate

particles

and

not

part

of

 

 

 

 

 

the

lattice,

usually

consist

of

silicates

of

aluminum,

 

 

 

 

 

magnesium,

or calcium

such

as olivine.f”j

 

 

 

 

 

 

The two major lattice impurities

found

in diamond

are nitrogen

and

boron.

These

two elements

are the neighbors

of carbon in the periodic

table.

They

have small

atomic

radii

and

fit

readily

within

the

diamond

structure.

Other

elemental

impurities

 

may also

be present

but only

in extremely

 

small

amounts

and

their effect

on the

properties

of the

material

is still

uncertain

but

probably

minor.t12]

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

 

Nitrogen.

Nitrogen

impurity

in diamond

is detected

and characterized

by

IR absorption

and

paramagnetic

 

resonance.

 

The majority of nitrogen

atoms

within

the

diamond

structure

 

are

arranged

 

in pairs as shown

in Fig.

11.8.[“] Isolated nitrogen atoms are

rarer.

Nitrogen

platelets

are

also

present and can be represented

as a quasi-planar

 

structure

within the cube

(100)

plane of the diamond

crystal.

 

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]

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