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Molybdenum Valence in Basaltic Silicate Melts: Effects of Temperature and Pressure

机译:玄武岩硅酸盐熔体中的钼价:温度和压力的影响

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The metal-silicate partitioning behavior of molybdenum has been used as a test for equilibrium core formation hypotheses (for example, 1-6). However, current models that apply experimental data to equilibrium core-mantle differentiation infer the oxidation state of molybdenum from solubility data or from multivariable coefficients from metal-silicate partitioning data (1,3,7). Molybdenum, a multi-valent element with a valence transition near the fO2 of interest for core formation (approx.IW-2) will be sensitive to changes in fO2 of the system and silicate melt structure. In a silicate melt, Mo can occur in either 4+ or 6+ valence state, and Mo(6+) can be either octahedrally or tetrahedrally coordinated. Here we present X-ray absorption near edge structure (XANES) measurements of Mo valence in basaltic run products at a range of P, T, and fO2 and further quantify the valence transition of Mo.

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