Tc. Wu et Wa. Bassett, DEVIATORIC STRESS IN A DIAMOND-ANVIL CELL USING SYNCHROTRON-RADIATIONWITH 2 DIFFRACTION GEOMETRIES, Pure and Applied Geophysics, 141(2-4), 1993, pp. 509-519
Deviatoric stress in a diamond anvil cell with gold as a pressure and
stress indicator is measured by two complementary techniques using syn
chrotron radiation. The first method employs a white X-ray beam using
energy dispersive X-ray diffraction. The incident X-ray beam is parall
el to the load axis and the diffraction pattern is recorded at a low t
wo-theta angle. Using powder diffraction patterns of polycrystalline g
old, we measured the elastic strain of two crystal planes oriented nor
mal to the diffraction vector. Stresses nearly parallel and perpendicu
lar to the load axis can be calculated by stress-strain tensor relatio
nship. The other method uses a monochromatic wiggler X-ray beam. In th
is case, the diamond cell is oriented so that the incident beam is per
pendicular to the load axis. The diffraction pattern is recorded on an
image plate area detector. Elastic strains responding to stresses per
pendicular and parallel to the load axis can be measured and stresses
of the same orientations can be calculated from the strain data. These
measurements provide a lower bound of the actual differential stresse
s in a diamond cell. With these techniques, we can measure stress dist
ribution in a less deviatoric gasketted sample and determine yield str
ength of mantle materials at high pressures and temperatures.