High pressure

For the related geology term, see Ultrahigh-pressure metamorphism. For the meteorology term, see High-pressure area. For the 1932 film, see High Pressure (film). For the Red Garland album, see High Pressure (Red Garland album).

In science and engineering, the study of high pressure examines its effects on materials and the design and construction of devices, such as a diamond anvil cell, which can create high pressure. High pressure usually means pressures of thousands (kilobars) or millions (megabars) of times atmospheric pressure (about 1 bar or 100 kilopascals).

History and overview

Percy Williams Bridgman received a Nobel Prize in 1946 for advancing this area of physics by two magnitudes of pressure (400 megapascals (MPa) to 40 gigapascals (GPa)). The founders of this field include also Harry George Drickamer, Tracy Hall, Francis P. Bundy, Leonid F. Vereschagin, and Sergey M. Stishov.

It was by applying high pressure as well as high temperature to carbon that synthetic diamonds were first produced alongside many other interesting discoveries. Almost any material when subjected to high pressure will compact itself into a denser form; for example, quartz (also called silica or silicon dioxide) will first adopt a denser form known as coesite, then upon application of even higher pressure, form stishovite. These two forms of silica were first discovered by high-pressure experimenters, but then found in nature at the site of a meteor impact.

Chemical bonding is liable to change under high pressure, when the P * V term in the free energy becomes comparable to the energies of typical chemical bonds at around 100 GPa. Among the most striking changes are metallization of oxygen at 96 GPa (rendering oxygen a superconductor), and transition of sodium from a nearly-free-electron metal to a transparent insulator at ~200 GPa. At ultimately high compression, however, all materials will metallize (see metallization pressure).‍

High-pressure experimentation has led to the discovery of the types of minerals which are believed to exist in the deep mantle of the Earth, such as silicate perovskite, which is thought to make up half of the Earth's bulk, and post-perovskite, which occurs at the core-mantle boundary and explains many anomalies inferred for that region.

Pressure "landmarks"

• Typical pressures reached by large-volume presses: up to 30–40 GPa
• Pressures that can be generated inside diamond anvil cells: ~1000 GPa‍
• Pressure at center of the Earth: 364 GPa
• Highest pressures ever achieved in shock waves: over 100 terapascals (100,000 GPa)‍

See also

• Metallization pressure
• Synthetic diamond – Diamond created by controlled processes
• D-DIA – Apparatus used for high pressure and high temperature deformation experiments
• Extreme pressure additive

Further reading

• Hazen, Robert M. (1993). The New Alchemists: Breaking Through the Barriers of High Pressure. New York: Times Books. ISBN 978-0-8129-2275-2. LCCN 93015703. OCLC 1150816525. OL 26486578M. ARK ark:13960/t6h173t03.