概括
射线吸收光谱显示,Fe2+) 协调率从晶体费亚利特中的6降至Fe2SiO4液体中的4. 这种结构变化影响了地球上的融化特性和元素分区.
科学领域:
- 地质化学 地质化学
- 材料科学 材料科学 材料科学
- 矿物物理 矿物物理
背景情况:
- 了解酸盐化的结构对于解释地球上的地物理观测和地化学过程至关重要.
- 铁 (Fe) 是许多地质材料的关键组成部分,其协调状态显著影响融特性.
- 以前的酸盐液体中的Fe2+模型在相关温度和压力下缺乏详细的结构信息.
研究的目的:
- 通过使用X射线吸收光谱学来确定化Fe(2) SiO(4) (fayalite) 中Fe(2+) 的局部结构环境.
- 为了研究化时协调号和Fe2+) -O键长度的变化.
- 开发一个结构模型Fe(2+) 在橄素组成的融及其对地质系统的影响.
主要方法:
- 进行X射线吸收光谱 (XAS) 对Fe(2) SiO(4) 液体在1575 K和10−4 GPa时进行.
- 分析涉及对液体结构中的不协调性进行核算.
- 对光谱数据与结点上的晶体法雅石进行比较.
主要成果:
- 在Fe(2) SiO(4) 液体中Fe(2+) -O 键的长度为1.98 ± 0.02 Å,比晶体费亚利特要短得多 (约1.98 ± 0.02 Å). 2.22 Å) 的时间.
- 平均Fe2+) 协调数从晶体法雅石中的6个下降到液体的4个.
- 这种协调变化类似于某些离子盐的化诱导的变化.
结论:
- 基于观察到的协调下降,开发了一种Fe2+中等范围结构环境的模型.
- 这些发现解释了Fe(2) SiO(4) 液体的关键性质,包括密度,粘度和Fe-Ni分区.
- 该模型对理解地球地和地幔中化的酸盐有意义.
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