Abstract
Chemical diffusion of F and Cl has been experimentally determined in a rhyodacitic melt obtained from remelting a sample of Hekla pumice (Iceland). Diffusion couple experiments were conducted in a vertical tube furnace over a temperature range of 750–950 °C and in air for durations of 1 to 35 days. Concentration profiles of F and Cl were obtained for the quenched samples using an electron microprobe.
Fluorine and chlorine exhibit Arrhenian behavior over the range of temperature investigated here. The pre-exponential factors of F and Cl are D0(F) = 4.3 × 10-4 and D0(Cl) = 1.6 × 10-5 m2/s. Fluorine diffusion coefficients vary in the order of 1 × 10-15 to 1 × 10-13 m2/s, whereas Cl diffusivity is up to two orders of magnitude slower. The activation energies for F and Cl diffusivities are equal within error at 223 ± 31 and 229 ± 52 kJ/mol, respectively.
The difference in diffusivity between F and Cl is particularly pronounced in the melt of our study, compared to results obtained for other magmatic melt compositions. This means that the potential for diffusive fractionation exists and may occur especially under conditions of magma ascent and bubble growth, as this would favor partitioning of the relatively fast-diffusing halogens into growing bubbles, due to H2O exsolution. A dependence of diffusivity on atomic radius observed here is enhanced over that observed in more basic, less viscous melts, indicating that diffusive fractionation is more likely to be pronounced in more silicic, more viscous systems. A proper parameterization and modeling of diffusive fractionation of halogens in actively degassing volcanic systems thus holds the potential of serving as a tool for quantifying the processes responsible for volcanic unrest.
Acknowledgments
We thank B. Scheu, U. Küppers, and K.-U. Hess for their assistance during sample preparation and N. Groschopf and S. Buhre for their assistance with electron microprobe analyses. B. Watson, H. Balcone-Boissard, and one anonymous reviewer are thanked for their insightful comments that helped to improve this paper.
Funding
This research is part of the Ph.D. thesis of Y. Feisel and is supported a fellowship of the Gutenberg Research College of the Johannes Gutenberg-University of Mainz to D.B. Dingwell. Additional support was provided by the VAMOS research center of the Johannes Gutenberg-University.
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Articles in the same Issue
- Crossroads in Earth and Planetary Materials
- Computer modeling of apparently straight bond angles: The intriguing case of all-silica ferrierite
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Articles in the same Issue
- Crossroads in Earth and Planetary Materials
- Computer modeling of apparently straight bond angles: The intriguing case of all-silica ferrierite
- Composite materials based on zeolite stilbite from Faroe Islands for the removal of fluoride from drinking water
- The Italian Solfatara as an analog for Mars fumarolic alteration
- Change of crackling noise in granite by thermal damage: Monitoring nuclear waste deposits
- Constraining the timing and character of crustal melting in the Adirondack Mountains using multi-scale compositional mapping and in-situ monazite geochronology
- Melting in the Fe-FeO system to 204 GPa: Implications for oxygen in Earth’s core
- Controls on tetrahedral Fe(III) abundance in 2:1 phyllosilicates
- Stability, composition, and crystal structure of Fe-bearing Phase E in the transition zone
- Enrichment of manganese to spessartine saturation in granite-pegmatite systems
- Al and Si diffusion in rutile
- Sound velocity of neon at high pressures and temperatures by Brillouin scattering
- A Cr3+ luminescence study of natural topaz Al2SiO4(F,OH)2 up to 60 GPa
- Two generations of exsolution lamellae in pyroxene from Asuka 09545: Clues to the thermal evolution of silicates in mesosiderite
- Crystallographic and fluid compositional effects on the halogen (Cl, F, Br, I) incorporation in pyromorphite-group minerals
- Diffusion of F and Cl in dry rhyodacitic melt