Diamond one of the forms of carbon
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Diamond is one of the two best known forms (or allotropes) of
carbon, whose hardness and high dispersion of light make it useful
for industrial applications and jewelry (the other equally well
known allotrope is graphite). Diamonds are specifically renowned as
a mineral with superlative physical qualities - they make excellent
abrasives because they can only be scratched by other diamonds,
which also means they hold a polish extremely well and retain
luster. About 130 million carats (26,000 kg) are mined annually,
with a total value of nearly USD $9 billion. |
The name "diamond" derives from the ancient
Greek adamas (αδάμας; "invincible"). They have been
treasured as gems since their use as religious icons in
India at least 2,500 years ago—and usage in drill bits and
engraving tools also dates to early human history.
Popularity of diamonds has risen since the 19th century
because of increased supply, improved cutting and polishing
techniques, and growth in the world economy. They are
commonly judged by the "four Cs": carat, clarity, color, and
cut. Although nearly four times the mass of natural diamonds
are produced as synthetic diamond each year, the vast
majority of synthetic diamond production remains small,
imperfect diamonds suitable only for industrial-grade use.
Most natural diamonds originate from central and southern
Africa, although significant sources of the mineral have
been discovered in Canada, India, Russia, Brazil, and
Australia. They are generally mined from volcanic pipes,
which are deep in the Earth where the high pressure and
temperature enables the formation of the crystals. The
mining and distribution of natural diamonds are subjects of
frequent controversy—such as with concerns over the sale of
conflict diamonds by African paramilitary groups. There are
also allegations that the De Beers Group misuses its
dominance in the industry to control supply and manipulate
price via monopolistic practices, although in recent years
the company's market share has dropped to below 50%.
Diamond is a transparent crystal of pure carbon consisting
of tetrahedrally bonded carbon atoms. Humans have been able
to adapt diamonds for many uses because of the material's
exceptional physical characteristics. Most notable among
these properties are the extreme hardness of diamond, its
high dispersion index, and high thermal conductivity. These
properties form the basis for most modern applications of
diamond.
Diamonds typically crystallize in the face-centered cubic
crystal system and consist of tetrahedrally bonded carbon
atoms. The unit cell of diamond has a two atom basis at
(0,0,0) and (1/4,1/4,1/4), which means half of the atoms are
at lattice points and the other half are offset by
(1/4,1/4,1/4), where 1 is the length of a side of the unit
cell.
The tetrahedral arrangement of atoms in a diamond crystal is
the source of many of diamond's properties. Graphite,
another allotrope of carbon, has a rhombohedra crystal
structure and as a result shows dramatically different
physical characteristics — contrary to diamond, graphite is
a very soft, dark gray, opaque mineral. Other elements of
the carbon group such as silicon have forms analogous to
diamond.
Lonsdaleite is a polymorph of diamond (and a distinct
mineral species) that crystallizes with hexagonal symmetry;
it is rarely found in nature, but is characteristic of
synthetic diamonds. A cryptocrystalline variety of diamond
is called carbonado. A colorless, grey or black diamond with
a tiny radial structure is a spherulite.
Diamond is the hardest known naturally occurring material,
scoring 10 on the relative Mohs scale of mineral hardness
and having an absolute hardness value of between 167 and 231
gigapascals in various tests. Diamond's hardness has been
known since antiquity, and is the source of its name.
However, aggregated diamond nanorods, an allotrope of carbon
first synthesized in 2005, are now believed to be even
harder than diamond.
The hardest diamonds in the world are diamonds from the New
England area in New South Wales, Australia. These diamonds
are generally small, perfect to semi perfect octahedral, and
are used to polish other diamonds. Their hardness is
considered to be a product of the crystal growth form, which
is single stage growth crystal. Most other diamonds show
more evidence of multiple growth stages, which produce
inclusions, flaws and defect planes in the crystal lattice
all of which affect their hardness (Taylor et al. 1990).
Industrial use of diamonds has historically been associated
with their hardness; this property makes diamond the ideal
material for cutting and grinding tools. It is one of the
most known and most useful of more than 3,000 known
minerals. As the hardest known naturally occurring material,
diamond can be used to polish, cut, or wear away any
material, including other diamonds. Common industrial
adaptations of this ability include diamond-tipped drill
bits and saws, or use of diamond powder as an abrasive.
Other specialized applications also exist or are being
developed, including use as semiconductors: some blue
diamonds are natural semiconductors, in contrast to most
other diamonds, which are excellent electrical insulators.
Industrial-grade diamonds are either unsuitable for use as
gems or synthetically produced, which lowers their price and
makes their use economically feasible. Industrial
applications, especially as drill bits and engraving tools,
also date to ancient times.
The hardness of diamonds also contributes to its suitability
as a gemstone. Because it can only be scratched by other
diamonds, it maintains its polish extremely well, keeping
its luster over long periods of time. Unlike many other
gems, it is well-suited to daily wear because of its
resistance to scratching—perhaps contributing to its
popularity as the preferred gem in an engagement ring or
wedding ring, which are often worn every day.
Unlike hardness, which only denotes resistance to
scratching, diamond's toughness is only fair to good.
Toughness relates to a material's ability to resist breakage
from forceful impact. As with any material, the macroscopic
geometry of a diamond contributes to its resistance to
breakage. Diamond is therefore more fragile in some
orientations than others.
Diamonds occur in a variety of transparent hues — colorless,
white, steel, blue, yellow, orange, red, green, pink,
brown—or colored black. Diamonds with a detectable hue to
them are known as colored diamonds. If the color is strong
enough, a stone may be referred to as a fancy colored
diamond by the trade. Colored diamonds contain impurities or
structural defects that cause the coloration, while pure or
nearly pure diamonds are transparent and colorless. Most
diamond impurities replace a carbon atom in the crystal
lattice. The most common impurity, nitrogen, causes a slight
to strong yellow coloration depending upon the type and
concentration of nitrogen present.
At surface air pressure (one atmosphere), diamonds are not
as stable as graphite, and so the decay of diamond is
thermodynamically favorable (ΔG = −2.99 kJ / mol). Diamonds
will burn at approximately 800 degrees Celsius, providing
that enough oxygen is available. This was shown in the late
18th century, and previously described during Roman times.
However, owing to a very large kinetic energy barrier,
diamonds are metastable; under normal conditions, it would
take an extremely long time (possibly more than the age of
the Universe) for diamond to decay into graphite.
Diamonds exhibit a high dispersion of visible light. This
strong ability to split white light into its component
colors is an important aspect of diamond's attraction as a
gemstone, giving it impressive prismatic action that results
in so-called fire in a well-cut stone. The luster of a
diamond, a characterization of how light interacts with the
surface of a crystal, is brilliant and is described as
adamantine, which simply means diamond-like. This is owed to
their high refractive index of 2.417 (at 589.3 nm), which
causes total internal reflection to occur. Some diamonds
exhibit fluorescence of various colors (predominately blue)
under long wave ultraviolet light. Nearly all diamonds
fluoresce bluish-white, yellow or green under X-rays and
this property is used extensively in mining to separate the
fluorescing diamond from the non-fluorescing rock. Most
diamonds show no fluorescence although colored diamonds show
a wider range of fluorescence than the blue fluorescence
normally observed in clear diamonds
Except for most blue diamonds, which are semiconductors,
diamonds are good electrical insulators. Blue diamonds owe
their semi conductive property to boron impurities, which
act as a doping agent and cause p-type semiconductor
behavior. Blue diamonds which are not boron-doped, such as
those recently recovered from the Argyle diamond mine in
Australia that owe their color to an overabundance of
hydrogen atoms, are not semiconductors.
Unlike most electrical insulators, diamond is a good
conductor of heat because of the strong covalent bonding
within the crystal. Most natural blue diamonds contain boron
atoms which replace carbon atoms in the crystal matrix, and
also have high thermal conductivity. Specially purified
synthetic diamond has the highest thermal conductivity
(2000–2500 W/(m·K), five times more than copper) of any
known solid at room temperature. Because diamond has such
high thermal conductance it is already used in semiconductor
manufacture to prevent silicon and other semi conducting
materials from overheating. |
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