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handbook of carbon, graphite, diamond and fullerenes

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12<br />

Natural <strong>and</strong> High-Pressure Synthetic<br />

Diamond<br />

1.0 INTRODUCTION<br />

Rough <strong>diamond</strong>s, that is, uncut <strong>and</strong> unpolished, were known <strong>and</strong><br />

prized in antiquity. They were first reported in India 2700 years ago. From<br />

India, <strong>diamond</strong> trading moved gradually westward through Persia <strong>and</strong> the<br />

Roman Empire. However the full beauty <strong>of</strong> <strong>diamond</strong> was not uncovered<br />

until faceting <strong>and</strong> polishing techniques were developed in the 14th <strong>and</strong> 15th<br />

centuries. A detailed history <strong>of</strong> <strong>diamond</strong> is given in Refs. 1 <strong>and</strong> 2.<br />

Unlike <strong>graphite</strong> <strong>and</strong> <strong>carbon</strong> materials, <strong>diamond</strong> is very rare <strong>and</strong>, with<br />

opal <strong>and</strong> ruby, considered the most valuable mineral, known the world over<br />

as a gemstone <strong>of</strong> perfect clarity, brilliance, hardness, <strong>and</strong> permanence.<br />

Diamond is produced in nature at high pressure <strong>and</strong> temperature in<br />

volcanic shafts. The high-pressure synthesis essentially duplicates this<br />

natural process <strong>and</strong> both materials, the natural <strong>and</strong> the synthetic, have<br />

similar properties <strong>and</strong> are reviewed together in this chapter.<br />

2.0 NATURAL DIAMOND<br />

2.1 Occurrence <strong>and</strong> Formation <strong>of</strong> Natural Diamond<br />

The two major allotropes <strong>of</strong> the element <strong>carbon</strong>, <strong>graphite</strong> <strong>and</strong> <strong>diamond</strong>,<br />

occur in igneous rocksJ 3 ' As seen in Ch. 11, at ordinary pressures<br />

278

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