Glass shows 'memory' under severe pressure.Glass shows 'memory' under severe pressure Molten sand, if cooled quickly enough, will harden before its silicon dioxide silicon dioxide: see silica. (SiO2) A hard, glassy mineral found in such materials as rock, quartz, sand and opal. In MOS chip fabrication, it is used to create the insulation layer between the metal gates of the top layer and the silicon elements below. molecules realign re·a·lign tr.v. re·a·ligned, re·a·lign·ing, re·a·ligns 1. To put back into proper order or alignment. 2. To make new groupings of or working arrangements between. into an ordered crystalline arrangement. That's one way of making glass. But two researchers find that an alternative method yields glasses that retain a "memory" of their original crystal structure and can actually revert to it. Geophysicist Raymond Jeanloz Raymond Jeanloz is a professor of earth and planetary science and of astronomy at the University of California, Berkeley. Educated at the California Institute of Technology, Amherst College and at Deep Springs College, he has contributed research fundamental to understanding of the of the University of California, Berkeley The University of California, Berkeley is a public research university located in Berkeley, California, United States. Commonly referred to as UC Berkeley, Berkeley and Cal , and graduate student Michael B. Kruger introduce their "memory glass" in the Aug. 10 SCIENCE. The team's pressure-based technique involves a diamond-anvil cell that can subject materials to pressures thousands or even millions of times greater than external atmospheric pressures. First, Jeanloz and Kruger surround their crystals with a fluid to ensure even pressure distribution around the samples, in this case the berlinite form of aluminum phosphate. When the pressure in the diamond-anvil cell reaches at least 150,000 atmospheres -- corresponding to the pressure about 250 miles below the Earth's surface Noun 1. Earth's surface - the outermost level of the land or sea; "earthquakes originate far below the surface"; "three quarters of the Earth's surface is covered by water" surface -- the aluminum and phosphate ions edge away from their crystalline sites into an amorphous arrangement. At these pressures, the X-ray diffraction pattern diffraction pattern The interference pattern that results when a wave or a series of waves undergoes diffraction, as when passed through a diffraction grating or the lattices of a crystal. indicative of crystalline order disappears. Changes in the way the material absorbs infrared radiation also suggest a crystal-to-glass transition, the researchers report. But to their surprise, the ions snap back into their original crystalline places when the pressure in the cell falls below 500 atmospheres. Jeanloz conjectures that the memory effect of aluminum phosphate, and of several other crystals tested, depends on the experiment's room-temperature conditions, which probably prevent the squeezed ions from wandering more than a smidgen from their original sites. So when the pressure goes down, the ions simply pop back into their thermo-dynamically favored places. The high temperatures used in conventional glass-making send the crystal's ions or molecules too far out of line to "remember" where they started, he says. "The recrystallization recrystallization, n the return of a wrought metal to crystalline form because of excessive cold working or excessive application of heat. recrystallization of an amorphous phase upon decompression is very intriguing," remarks Russell J. Hemley of the Carnegie Institution of Washington |
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