Ambient and high pressure single crystal x-ray studies of pyrope and synthetic ferric majorite

The mineral garnet is widely accepted as a major constituent of Earth's upper mantle and transition zone. As such, understanding of the state of the material at high pressures and temperatures will increase our ability to correlate seismic data with the mineralogy in these regions of Earth's interior. Studies of varied compositions of garnet at ambient conditions may enhance our understanding of solid-solution energetics, and yield predictive power concerning element partitioning among various minerals at different depths within Earth. This study began with structure refinements at ambient conditions of eighteen natural and two synthetic garnets, nominally in the pyrope-grossular-almandine ternary system. The natural, nearly-pure pyrope sample of this group was then used in developing the techniques necessary for high-pressure structure refinements. For high pressure work, a diamond anvil pressure cell (DAC) was loaded with the sample and mounted on an 18 kW rotating anode four-circle diffractometer. Unit cells and oxygen positional parameters of the pyrope sample were refined at five pressures to 9.9 GPa. The data were in agreement with those of other studies, and extended by 40% the pressure range achieved previously. The zero-pressure bulk modulus, K = 176 GPa, with K;Following the high pressure pyrope study, synthetic samples of Fe-bearing majoritic garnet became available. These samples are of particular interest because they were grown at transition zone conditions and coexisted with a hydrous wadsleyite phase. The hydration state of earth's mantle is a topic of much current research, and samples such as these will provide information necessary to the placement of constraints on the degree of hydration actually present. The structures of five majorite samples from three different synthesis runs were refined at ambient conditions, and two of these samples were analyzed using Mossbauer spectroscopy. Fe...