Alumina is an important technological material
due to its presumed stability over a wide range of pressures. This stability lends
itself to several important applications in high-pressure physics, including use
in the diamond-anvil cell. Over the last couple of decades, the diamond-anvil cell
has emerged as a work horse of high-pressure research, enabling researchers, for
the first time, to measure solid properties at pressures corresponding to the earth’s
mantle and below. The diamond-anvil cell, an apparatus used to generate large pressures,
is a chamber less than one hundredth of a millimeter in diameter in which scientists
place ruby, or chromium-doped alumina, along with the material to be studied.
Ruby plays an important role in such experiments, serving as the basis for a secondary
pressure calibrant, known as the ruby scale. Ruby is obtained by substituting a few
aluminum atoms in alumina with chromium (color centers), which provides a source
of fluorescence when excited by light. The wavelength of this fluorescence depends
directly on the pressure in the ruby. By measuring the wavelengths of the fluorescence
emissions, researchers can determine the pressure inside the diamond-anvil cell.
The reliability of the ruby scale, then, depends on the stability of the alumina
structure throughout the pressures studied in a particular experiment. If alumina
became unstable, it would transform into another phase at higher pressures. That
phase would, in turn, have a different structure from the low-pressure phase, and
this structural change could affect the reliability of the ruby scale. As yet, no
phase transformation of alumina has been experimentally observed. However, calculations
have predicted two pressure-induced transformations of alumina from its low-pressure
phase, known as corundum, to high pressure polymorphs. These predicted polymorphs
are the Rh2O3 (II) phase and an orthorhombic perovskite phase. The figures below
depict the different molecular structures of these three phases. Dr. Renata M. Wentzcovitch,
research fellow Kendall T. Thomson, and post-doc Wenhui Duan, of the University’s
Department of Chemical Engineering and Materials Science, are using a technique called
first principle-molecular dynamics (FPMD) to predict such transformations. Their
procedure calculates the electronic energy, forces, and stress in a solid-state configuration
quantum mechanically (by first principles) and solves for the fully-relaxed ground-state
configuration (in which the atomic positions in the solid are allowed to “relax”
into positions that give the lowest energy) at arbitrary pressures. By comparing
the calculated enthalpies of the corundum phase and other possible high-pressure
phases, accurate predictions of transformation pressures have been obtained.
The work is providing, for the first time, predicted phase stabilities of alumina
using fully relaxed geometries. By Wentzcovitch, Thomson and Duan’s method, the corundum
phase, Al2O3, is predicted to undergo a transformation to another structure, called
Rh2O3 (II), at pressures corresponding to those found midway through the earth’s
lower mantle. A further transformation to an orthorhombic perovskite phase is also
predicted at even greater pressures of approximately 223 GPa. Because pressures of
well over 500 GPa have been obtained in diamond-anvil cell experiments recently,
the predicted phase behavior of alumina could be important in pinning down the exact
pressure in these experiments. It is possible that, due to the nature of reconstructive
phase transformations, the observed alumina phase in a particular experiment depends
strongly on the thermal history of the ruby chips (the ruby scale is therefore presumed
to be sensitive to the thermal history as well). Confirmation of whether or not the
Rh2O3 (II) phase is even observable is hampered by limitations in high-pressure x-ray
technology. The structural similarity between corundum and Rh2O3 (II) results in
very similar X-ray spectra. It is therefore quite possible that small amounts of
the Rh2O3 (II) phase could go undetected in high-pressure X-ray measurements |
These figures show the predicted phase tranformations of alumina. Al2O3,
as its molecular structure changes due to pressure.
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Figure 1
Corundum, the low-pressure structure of alumina
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Figure 2
Rh2O3(II), a predicted high-pressure polymorph of alumina.
The corundum phase is predicted to transform tothis phase at approximately 78 GPa
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Figure 3
Orthorhombic perovskite, another high-pressure polymorph of alumina. Rh2O3(II)
phase is predicted to transform to this phase at approximately 223 GPa
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The specific effect of these phase transformations on the ruby scale is the current
focus of this research. By simulating a “supercell” of 80 atoms, and including chromium
defects, Duan is evaluating the response of ruby fluorescence lines to changing pressure
and phase composition. |