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Metal-silicate silicon isotopic fractionation and the composition of the bulk Earth

机译:金属 - 硅酸盐硅同位素分级和散装地球的组成

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摘要

The difference in the Si isotopic composition between the Earth and primitive meteorites had been used to constrain the amount of Si in the Earth's core. However, there is presently a debate on the magnitude of the isotopic fractionation between metal and silicates as function of temperature based on experimental data. Here, we use a natural sample, an enstatite meteorite, Itqyi, as a natural experiment to determine an independent Si isotopic fractionation factor between metal and silicate. We determined the temperature of equilibrium between metal and silicate as well as the Si isotopic composition between the phases. We find that the dependence of Si isotopes with temperature to be:
机译:地球和原始陨石之间的Si同位素组成的差异已被用来限制地球核心中的Si量。 然而,目前存在关于金属和硅酸盐之间的同位素分馏的大小的争论,如实验数据的温度的功能。 在这里,我们使用天然样本,enstatite陨石,Itqyi作为自然实验,以确定金属和硅酸盐之间的独立Si同位素分级因子。 我们确定了金属和硅酸盐之间的平衡温度以及相位之间的Si同位素组成。 我们发现Si同位素与温度的依赖性是:

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