Salle 2, Site Marcelin Berthelot
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Diamond-structured carbon is a material with exceptional properties. From the macroscopic to the nanoscopic scale, we present the various synthetic diamonds, their synthesis methods and properties. Natural diamonds are formed in the craton under high pressures and temperatures (P = 43,000 atmospheres, T = 1,000-1,500°C) and date, for the most part, from the Archean age (-2.5 billion years). The vast majority of diamonds crystallized at depths of between 150 and 250 km, and were brought to the earth's surface by kimberlite volcanic eruptions. This precious carbon stone has been mined for 6,000 years in India, Brazil and Africa. In the course of the 20thcentury , the development and use of diamonds on an industrial scale was made possible by synthetic diamonds obtained by high-pressure, high-temperature processes. These diamonds, synthesized on a macroscopic scale (micron or millimeter sizes), have exceptional mechanical, thermal, acoustic and optical properties, in particular their very high hardness and very low coefficient of friction, which enable them to be used in drill bits in the oil and gas industry, in cutting, grinding and polishing tools, in microelectromechanical systems and in surgical scalpels for ophthalmic and neurological surgery. Its good thermal conductivity enables synthetic diamond to make a valuable contribution in all types of electronic and electrical applications where heat build-up can destroy delicate circuits or seriously impair performance. Its acoustic properties make diamond an essential element in high-performance loudspeakers. This material has the widest spectral range, from ultraviolet to far infrared, and from microwaves to millimeter waves. As a result, it is often used in the production of optical windows and laser optics. Diamond is also used for industrial and domestic electrochemical water treatment. In particular, synthetic diamond anodes can be used to produce ozone on a scale suitable for domestic use.