Prediction of equilibrium Li isotope fractionation between minerals and aqueous solutions at high P and T: an efficient ab initio approach
Piotr M. Kowalski, Sandro Jahn

TL;DR
This paper introduces an efficient ab initio method to predict lithium isotope fractionation between minerals and aqueous solutions at high P and T, aligning well with experimental data and providing atomic-scale insights.
Contribution
The paper presents a novel, unified ab initio approach for calculating isotope fractionation in minerals and fluids under high P and T conditions, applicable to various states.
Findings
Accurately predicts lithium isotope fractionation direction and magnitude.
Agrees within 1 permil with experimental values.
Provides atomic-scale understanding of fractionation mechanisms.
Abstract
The mass-dependent equilibrium stable isotope fractionation between different materials is an important geochemical process. Here we present an efficient method to compute the isotope fractionation between complex minerals and fluids at high pressure, P, and temperature, T, representative for the Earth's crust and mantle. The method is tested by computation of the equilibrium fractionation of lithium isotopes between aqueous fluids and various Li bearing minerals such as staurolite, spodumene and mica. We are able to correctly predict the direction of the isotope fractionation as observed in the experiments. On the quantitative level the computed fractionation factors agree within 1.0 permil with the experimental values indicating predictive power of ab initio methods. We show that with ab initio methods we are able to investigate the underlying mechanisms driving the equilibrium…
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