Ge isotopic equilibrium fractionation between Ge-containing ferrihydrite and the aqueous solution


Ge isotopic equilibrium fractionation between Ge-containing ferrihydrite and the aqueous solution


Peng-dong Wang

School of Earth Science and Engineering, Hebei University of Engineering, Handan 056038, China


Since Ge has a strong affinity for Fe, iron oxyhydroxide is assumed to be one of the potential “missing sinks” of Ge. Ferrihydrite is commonly found in soil and sediments and has a strong affinity for heavy metals. In this study, the first principle method based on density functional theory was used to optimize the geometry of Ge-containing ferrihydrites and H4GeO4 aqueous solution molecular clusters at B3LYP/6-311G(d) level. Solvation effects are treated by “water-droplet” method. Finally, at 298.15 K we obtained the Ge isotopic equilibrium fractionation between Ge-containing ferrihydrites and H4GeO4 aqueous solution, Δ74/70Geferrihydrite-aq= -1.97‰. It enriches the document of Ge isotopic fractionation and helps to assist the study of Ge global cycle.


Keywords: Ge isotopes; isotopic equilibrium fractionation; first-principles calculation; ferrihydrite

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How to cite this article:

Peng-dong Wang. Ge isotopic equilibrium fractionation between Ge-containing ferrihydrite and the aqueous solution. American Journal of Basic and Applied Sciences, 2022; 5:25. DOI:10.28933/ajbas-2022-10-2505


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