概括
在太阳系中常见的铁磁橄可能不是连续的固体溶液. 来自Divnoe石的自然样本显示,在低温下存在混合性差距的证据.
科学领域:
- 矿物学是什么?矿物学是什么?
- 地质化学 地质化学
- 行星科学 行星科学
背景情况:
- 铁磁橄是太阳系中广泛存在的矿物质.
- 传统上,它被视为一种连续的固体溶液.
- 热力学模型表明,在低温下存在潜在的混合性差距.
研究的目的:
- 为了调查铁磁橄固体溶液中混合性差距的存在.
- 提供支持或反对拟议的低温混合性差距的直接证据.
主要方法:
- 对天然铁磁橄样品的分析.
- 在橄结构中检查溶液外面的叶片.
主要成果:
- 迪文诺石中含有铁磁橄,具有明显的溶解板状.
- 这些叶片呈现出不同组成的不同阶段.
- 这为混合性差距提供了直接证据.
结论:
- 这项研究证实,在低温下铁橄酸盐固体溶液中存在混合性差距.
- 这一发现挑战了长期以来关于连续固体溶液行为的观点.
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