Externally-driven charge transfer in silicates at high pressure and temperature: A XANES study

12Citations
Citations of this article
26Readers
Mendeley users who have this article in their library.
Get full text

Abstract

Modest perturbations induced by an externally-applied electric field can generate significant variations in effective oxygen fugacity in high temperature silicates. This result has at least two-fold importance: first, it is a new petrologic technique to examine the behavior of a single sample under a large range of effective oxygen fugacity; and second, it is a mechanism for planetary electric fields to generate potentially significant chemical heterogeneities within planetary interiors. The redox state of Fe and V within a partially melted basaltic andesite was manipulated in situ in a piston-cylinder experiment with a DC power supply providing a source and sink of electrons to the sample. A 1 V electrical potential difference was applied across vanadium-doped synthetic basalt samples for 24 h. at 20 kbar and 1400 °C in a specially-designed piston cylinder sample assembly. Three experiments were performed: a control sample with no applied voltage, one with bottom ground and top anode (+ 1 V), and a third with top ground and bottom anode (+ 1 V). Synchrotron-based X-ray absorption near edge structure spectroscopy (XANES) was used to provide maps of iron and vanadium oxidation states with 5 μm × 5 μm spatial resolution throughout the recovered samples. Systematic increasing oxidation states of V and Fe were observed approaching the anode. Oxidation states were mapped to corresponding local oxygen fugacities by comparison with a series of samples synthesized under known oxygen fugacity conditions from previous studies. Both Fe and V markers indicate that the 1 V potential drop across the sample induces effective oxygen fugacity perturbations of 10 orders of magnitude. Therefore, it is possible that the presence of modest poloidal electric fields (∼ 10- 6 V/m) within the Earth's outer core may provide an electrochemical driving force for localized charge transfer reactions in certain overlying mantle areas, generating local order-of-magnitude differences in effective oxygen fugacity. © 2007 Elsevier B.V. All rights reserved.

Cite

CITATION STYLE

APA

Kavner, A., Walker, D., Sutton, S., & Newville, M. (2007). Externally-driven charge transfer in silicates at high pressure and temperature: A XANES study. Earth and Planetary Science Letters, 256(3–4), 314–327. https://doi.org/10.1016/j.epsl.2006.12.020

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free