用丰富的酸矿的热态方程
1Center for High Pressure Research and Department of Geosciences, State University of New York at Stony Brook, Stony Brook, NY 11794, USA.
概括
地球地幔的同质性是通过比较实验室数据与地震发现来推断的. 关于含的矿的新数据表明,其性能有所不同,可能会改变我们对地幔组成的理解.
科学领域:
- 地质物理学 地质物理学
- 矿物物理 矿物物理
- 材料科学 材料科学 材料科学
背景情况:
- 地球地幔的化学均性是通过比较实验室状态方程与地震数据来评估的.
- 之前对MgSiO3矿的研究与一个均的地幔组成一致.
- (Al2O3) 是地球地幔相中的一个关键组成部分.
研究的目的:
- 为了研究对MgSiO3矿状态方程的影响.
- 为了确定含的矿是否会改变地幔化学同质性的推断.
- 改进地球下层地幔属性的模型.
主要方法:
- 实验室实验测量压力-体积-温度 (PVT) 数据.
- 状态参数方程的分析,包括散装模量.
- 实验数据与地震学观测数据的比较.
主要成果:
- 与没有的矿相比,含有5%分数Al2O3的酸呈现出不同的状态参数方程.
- 含的矿的散装模量在下层地幔条件下显著较小.
- 这些发现需要调整与地震观测相匹配的模型.
结论:
- 在MgSiO3矿中存在会影响其物理性质.
- 以前关于地幔均性的假设可能需要根据的影响进行修订.
- 准确地建模下层地幔需要将等杂质的影响纳入其中.
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