CALL FOR PROPOSALS:

ORGANIZERS

  • Harvey Thorleifson, Chair
    Minnesota Geological Survey
  • Carrie Jennings, Vice Chair
    Minnesota Geological Survey
  • David Bush, Technical Program Chair
    University of West Georgia
  • Jim Miller, Field Trip Chair
    University of Minnesota Duluth
  • Curtis M. Hudak, Sponsorship Chair
    Foth Infrastructure & Environment, LLC

 

Paper No. 8
Presentation Time: 10:20 AM

AMBIENT TEMPERATURE P-V EQUATION OF STATE FOR GARNET SAND OF PFEIFFER BEACH


COTTER, Erica L., Physics and Astronomy, Indiana University South Bend, 1700 Mishawaka Ave, South Bend, IN 46615 and SCOTT, Henry P., Physics and Astronomy, Indiana University South Bend, 1700 Mishawaka Ave, South Bend, IN 46634, elcotter@umail.iu.edu

Synchrotron powder X-ray diffraction analysis was performed on a natural beach-sand garnet from Pfeiffer Beach, located in Big Sur, California. The ambient-pressure lattice parameter, a, is 11.529 Å. The lattice parameter and, accordingly, unit-cell volume were determined through isothermal compression to 19 GPa in a symmetric diamond anvil cell, in which helium was used as a nearly-hydrostatic pressure-transmitting medium. The isothermal bulk modulus, K0T, was found to be 167.8 ± 2.7 GPa, using a second-order (i.e. dK/dP fixed at 4) Birch-Murnaghan equation of state. These results are consistent with previous elasticity measurements on a broad range of garnet compositions, and we will present our measurement in relation to prior work on bulk modulus - volume - cation valence systematics (e.g. Hazen et al., 1994).
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