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Diffusive fractionation of lithium and boron isotopes in silicate melts: a tool to study degassing in ascending magmas

Subject Area Mineralogy, Petrology and Geochemistry
Term from 2017 to 2021
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 349804343
 
Final Report Year 2022

Final Report Abstract

In this study the diffusivity and kinetic fraction of Li and B in a rhyolitic melt composition was determined for H2O-contents that are quite typical for natural magmas. These data do fill a gap in knowledge and clearly document the strong effect of H2O dissolved in silicate melts on the transport kinetics of these two elements. Based on these results, time windows for ascent-speedometers could be established that range from seconds to hours for Li, and from hours to weeks or months for B, depending on H2O-content of the melt. By decompression experiments with various decompression rates the evolution of Li and B contents and isotopes during bubble nucleation and growth was determined and provided insights to realistic situations of natural magma ascent and eruption and the chemical variations around vesicles that can be expected. With these data the predictive quality of numerical models on the chemical evolution of degassing and ascending magmas was assessed to point out their strengths and limits.

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