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Modelling of hydrogen permeation experiments in iron alloys : characterization of the accessible parameters : part II : the exit side Ghent University Vrije Universiteit Brussel
First-principles investigation of equilibrium iron isotope fractionation in Fe 1−xS x alloys at Earth's core formation conditions Vrije Universiteit Brussel
Iron is one of the most abundant non-volatile elements in the solar system. As a major component of planetary metallic alloys, its immiscibility with silicates plays a major role in planetary formation and differentiation. Information about these processes can be gained by studying the equilibrium Fe isotope fractionation between metal alloys and molten silicates at conditions of core formation. In particular, recent attention has been paid ...
Numerical interpretation to differentiate hydrogen trapping effects in iron alloys in the Devanathan-Stachurski permeation cell Ghent University Vrije Universiteit Brussel
Modelling of hydrogen permeation experiments in iron alloys : characterization of the accessible parameters : part I : the entry side Ghent University Vrije Universiteit Brussel
Electrochemical Modelling of the Hydrogen Absorption, Diffusion and Desorption in Iron Alloys Vrije Universiteit Brussel
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Lead isotopic analysis of copper alloy artifacts from Tell Tweini : changing ore sources from the early bronze age to the iron age? Ghent University
Identifying the geological provenance of an artifact, i.e. the origin of the ores used to produce a metal, provides important information on ancient relationships and connections, trade, and the movement of raw materials and/or objects. The initial approach to this provenance question applied elemental chemical analysis of artifacts and their proposed ore sources, but soon proved to be ineffective due to chemical heterogeneities in ore deposits ...