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Welcome
to the OSU Mineral Physics Research Group where we simulate
the
high-pressure, high-temperature conditions of the Earth's interior
using the
laser-heated diamond anvil cell (DAC). Current experimental
efforts
include: melting of metals at high pressure using isotopically marked
samples
for absolute determination of melt, solubility of volatile elements
(e.g. H, C)
in octahedrally-coordinated silicates, and high-pressure,
high-temperature
equations of state. Our work uses infrared laser heating,
synchrotron-based
high-temperature, high-pressure X-ray diffraction and infrared
spectroscopy,
laser-ablation (ICP-MS), nano-SIMS, Transmission Electron
Microscopy
(TEM), and Scanning Electron Microscopy (SEM). Contact Us: The School of Earth Sciences Other LinksOSU homepageOSU geology |
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