HR: 1340h
AN: MR13A-0062    [Abstracts]
TI: Rheological Studies of Komatiite Liquids by In-Situ Falling Sphere Viscometry
AU: * O Dwyer, L
EM: odwyer@geology.ucdavis.edu
AF: Dept. of Geology, Univ. of California, Davis, One Shields Avenue, Davis, CA 95616 United States
AU: Lesher, C E
EM: lesher@geology.ucdavis.edu
AF: Dept. of Geology, Univ. of California, Davis, One Shields Avenue, Davis, CA 95616 United States
AU: Baxter, G
EM: baxter@geology.ucdavis.edu
AF: Dept. of Geology, Univ. of California, Davis, One Shields Avenue, Davis, CA 95616 United States
AU: Clark, A
EM: anclark@ucdavis.edu
AF: Dept. of Geology, Univ. of California, Davis, One Shields Avenue, Davis, CA 95616 United States
AU: Fuss, T
EM: tihana@umr.edu
AF: Ceramic Enginneering Department, Univ. of Missouri - Rolla, Rolla, MO 64409 United States
AU: Tangeman, J
EM: tangeman@containerless.com
AF: Containerless Research, Inc, University Place, Evanston, IL 60201 United States
AU: Wang, Y
EM: wang@cars.uchicago.edu
AF: GSECARS-APS, ANL, Argonne, IL 60439 United States
AB: The rheological properties of komatiite liquids at high pressures and temperatures are being investigated by the in situ falling sphere technique, using the T-25 multianvil apparatus at the GSECARS 13 ID-D-D beamline at the Advanced Photon Source, ANL. The refractory and fluid nature of komatiite and other ultramafic liquids relevant to the Earth's deep interior, presents unique challenges for this approach. To reduce the density contrast between the melt and the marker sphere, and thus increase the Stoke's travel time, we have begun testing various composite spheres composed of refractory silicates and metals. Two successful custom designs are zirconia silicate mantled by Pt and Pt mantled by forsterite. These custom spheres contain sufficient Pt to absorb x-rays, while containing sufficient low-density refractory silicate so that marker sphere densities are in the range of 4-6 g/cc. These relatively more buoyant spheres increase travel time. These custom spheres, together with Re or Pt marker spheres, have been used to determine the viscosity of Gorgona anhydrous komatiite around 1600 ° C between 3.5 and 6 GPa. Initial experiments yield viscosities of 2.8 Pa s at 3.5 GPa, 5.3 Pa s at 4.6 GPa and 7.6 Pa s at 6 GPa. The observed positive pressure dependence of viscosity is consistent with recent results on pyrolite composition liquids and suggests that the activation volume for highly depolymerized melts will be positive for at least upper mantle conditions. The development of low-density, x-ray detectable marker spheres has applications in studies of melt density, whereby in situ detection of sink-float behavior during heating and compression cycles may be possible.
DE: 3630 Experimental mineralogy and petrology
DE: 3900 MINERAL PHYSICS
DE: 3954 X-ray, neutron, and electron spectroscopy and diffraction
SC: Mineral and Rock Physics [MR]
MN: Fall Meeting 2005