概括
这项研究使用微红外光谱学量化MgSiO(3) 矿中的微量. 这些发现表明,地球下层地幔中存在大量的气,与水球相似.
科学领域:
- 地质化学 地质化学
- 矿物物理 矿物物理
- 频谱学是一种光谱学.
背景情况:
- MgSiO(3) 矿是地球下层地幔中的主要矿物.
- 了解其微量元素含量,特别是,对于地幔的组成和动态至关重要.
- 名义上无水矿物质可以含有大量的.
研究的目的:
- 测量MgSiO的单晶中的微量含量.
- 为了研究这个地幔矿物中的分布和度.
- 为了将估计的下层地幔含量与地球水球进行比较.
主要方法:
- 使用微红外光谱学与同步红外光源.
- 分析了3483和3423厘米的吸收峰值,以确定氧化物存在.
- 基于光谱学数据的量化度.
主要成果:
- 在MgSiO(3) 矿中确定了两个明显的粉氧化吸收峰值.
- 确定的微量含量为700 +/- 170个原子,每10 (六) 个Si原子.
- 计算出这种度,集成在下层地幔上,大约是地球水球质量的12%.
结论:
- 矿含有可测量的和大量的微量.
- 下层地幔可能含有大量的气储备,影响地幔的性质.
- 这些发现需要重新评估地球内的水含量和循环.
相关概念视频
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