HR: 1340h
AN: MR13A-0055    [Abstracts]
TI: Density and Viscosity Measurement of Liquid FeS at High Pressure and High Temperature Using Synchrotron X-ray
AU: * Yu, T
EM: tony.yu@sunysb.edu
AF: Department of Geosciences and Mineral Physics Institute, Stony Brook University, Stony Brook, NY 11794-2100 United States
AU: Long, H
EM: hongbo.long@sunysb.edu
AF: Department of Geosciences and Mineral Physics Institute, Stony Brook University, Stony Brook, NY 11794-2100 United States
AU: Young, C
EM: ceyoung@gmail.com
AF: Department of Geosciences and Mineral Physics Institute, Stony Brook University, Stony Brook, NY 11794-2100 United States
AU: Wang, L
EM: liping.wang@sunysb.edu
AF: Department of Geosciences and Mineral Physics Institute, Stony Brook University, Stony Brook, NY 11794-2100 United States
AU: Chen, J
EM: jiuhua.chen@sunysb.edu
AF: Department of Geosciences and Mineral Physics Institute, Stony Brook University, Stony Brook, NY 11794-2100 United States
AB: From previous experimental and theoretical studies, sulfur has been considered one of the possible light elements in the core that might be responsible for the large density deficit when compared with the theoretical pure Fe core (Ganapathy and Anders, 1974; Ahrens and Jeanloz, 1987). Therefore, understanding the physical properties of liquid FeS will help us reveal the details of the Earth?|s core. This study focused on the liquid state of sulfur in iron due to sulfur?|s lack of amount in the mantle; easiness to alloy with iron; and the predicted 5 wt% ~10 wt% amount of this light element in the core (Ahrens, 1979; Sherman, 1997). Modern development of the multi-anvil high pressure apparatus limits the pressure range of the experiments (<30 GPa). It is somewhat low if comparing with the outer core pressure condition. Therefore, extrapolation of data derived at low pressure range to the condition of the outer core (>130 GPa) has to be applied, and may produce results that are far from the true numbers. However, at the point while the techniques are limited, studying the physical properties of the liquid-phase FeS at relatively low pressures still provides us a better picture of the physical behavior of the outer core comparing with data derived from solid state FeS experiments. Pervious studies on the viscosity of the Fe-FeS system (LeBlanc and Secco, 1996; Dobson et al., 2000; Urakawa et al., 2001; Secco et al., 2002) have presented different values of viscosity numbers with a maximum difference of two orders of magnitude. We have conducted the density measurements of liquid FeS (~36 wt% of S) up to 5.6 GPa in pressure and 1673K in temperature using the in-situ synchrotron-source x-ray absorption setup at Beamline X17B2, NSLS. The viscosity measurements were conducted by the x-ray radiograph technique combined with the falling sphere method. The falling sphere method applied at the experiment is suitable for liquids with viscosities between 10^-3 Pa-s and 10⁵ Pa-s (LeBlanc et al., 1999). We used tungsten spheres in our viscosity measurement experiments. We analyzed the sphere falling motion in the sample chamber at high pressure and high temperature. And by applying our density compression curve of liquid FeS to the Stokes?| viscometry method, we were able to derive the viscosity of liquid FeS.
DE: 3919 Equations of state
DE: 3924 High-pressure behavior
DE: 3954 X-ray, neutron, and electron spectroscopy and diffraction
SC: Mineral and Rock Physics [MR]
MN: Fall Meeting 2005