The electrical conductivity of albite feldspar: implications for oceanic lower crustal sequences and subduction zones

George M. Amulele, Anthony W. Lanati*, Simon M. Clark

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

Abstract

Volatile-sensitive electrical soundings are becoming more widely adopted with large nationwide arrays currently being acquired globally. This boom in new data is despite a number of key uncertainties relating to the electrical responses of a wide range of minerals that make up crustal regions. Complications include the influence of mineral chemistry, hydrous or nominally hydrous phases, and oxygen fugacity on charge-carrying ion activity within a mineral substrate. Feldspars are the most abundant mineral group in the Earth's crust, comprising about 60% of its mineral assemblages and are particularly prevalent within subduction zones and lower crustal sequences. These areas are known locations where ore systems are commonly rooted making them among the most widely studied regions in Earth. To date, Few studies exist that cover the electrical behavior of the intermediate feldspar mineral albite. In order to help address some of these issues and complications we have undertaken electrical conductivity investigations on a single crystal of gem-quality albite from Nuevo Casas Grande, Chihuahua, Mexico. Electrical conductivity measurements using impedance spectroscopy were performed at a pressure of 1 GPa and over a temperature range of 373 - 1273 K in a multi-anvil high-pressure apparatus. Experiments were carried out using different metal electrodes; molybdenum, nickel, and rhenium to vary the oxygen fugacity during the experiments. FTIR measurements of the starting and final materials confirm that the initial samples are completely dry but absorb an average of 67 ppm H2O by mass during the experiments from the surrounding pressure medium materials. We observe no correlation in the amount of water absorbed in the field sparing to the oxygen fugacity under water undersaturated conditions. Our investigations show that the activation enthalpy increases from ~ 0.77 eV to ~ 1.0 eV from the nominally hydrous to the completely dry feldspar. The activation enthalpy decreases with increasing oxygen fugacity for comparable water contents. An oxygen fugacity exponent of -0.069 is calculated at the nominal water content measured in the experiment, indicating an electrical conductivity mechanism that also involves the mobility of hydrogen. We observe no correlation in the amount of water absorbed in the field sparing to the oxygen fugacity under water undersaturated conditions. Our investigations show that the activation enthalpy increases from ~ 0.77 eV to ~ 1.0 eV from the nominally hydrous to the completely dry feldspar. The activation enthalpy decreases with increasing oxygen fugacity for comparable water contents. An oxygen fugacity exponent of -0.069 is calculated at the nominal water content measured in the experiment, indicating an electrical conductivity mechanism that also involves the mobility of hydrogen. We observe no correlation in the amount of water absorbed in the field sparing to the oxygen fugacity under water undersaturated conditions. Our investigations show that the activation enthalpy increases from ~ 0.77 eV to ~ 1.0 eV from the nominally hydrous to the completely dry feldspar. The activation enthalpy decreases with increasing oxygen fugacity for comparable water contents. An oxygen fugacity exponent of -0.069 is calculated at the nominal water content measured in the experiment, indicating an electrical conductivity mechanism that also involves the mobility of hydrogen. The activation enthalpy decreases with increasing oxygen fugacity for comparable water contents. An oxygen fugacity exponent of -0.069 is calculated at the nominal water content measured in the experiment, indicating an electrical conductivity mechanism that also involves the mobility of hydrogen. The activation enthalpy decreases with increasing oxygen fugacity for comparable water contents. An oxygen fugacity exponent of -0.069 is calculated at the nominal water content measured in the experiment, indicating an electrical conductivity mechanism that also involves the mobility of hydrogen.
Original languageEnglish
JournalAmerican Mineralogist
DOIs
Publication statusAccepted/In press - 2021

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