闪亮的结构色彩源于化石氨岩中纳米层的纳米隙反射
Naoki Hizukuri1, Yuri Oshima1, Yuta Yagi1
1School of Integrated Design Engineering, Faculty of Science and Technology, Keio University, 3-14-1 Hiyoshi, Kohoku-ku, Yokohama, 223-8522, Japan.
Scientific reports
|October 31, 2025
概括
阿莫莱特宝石中的鲜色彩源于化石中的纳米尺寸的空隙. 这些特定的层间纳米间隙 (约4纳米) 导致独特的光干扰,从而产生宝石.
科学领域:
- 古生物学的古生物学
- 材料科学 材料科学 材料科学
- 光学是什么?光学是什么?
背景情况:
- 阿莫莱特是一种来自加拿大阿尔伯塔省开采的化石氨石的宝石,呈现出鲜的色彩.
- 这种色彩归因于光线干扰对保存的真珠的干扰.
- 阿莫莱特独特的结构色彩背后的精确机制,将其与其他外结构区分开来,仍然不清楚.
研究的目的:
- 为了阐明Ammolite中观察到的生动结构颜色的根本原因.
- 为了区分Ammolite的光学特性与其他生物性结构颜色.
主要方法:
- 在Ammolite中对化石化纳克质层的纳米结构的分析.
- 研究光反射光谱及其与结构特征的相关性.
主要成果:
- 在化石的阿拉贡石板中确定了特定的间层纳米间隙 (大约4nm).
- 证明这些纳米间隙的均层化周期对于生动的颜色出现至关重要.
- 建立了层厚度和由此产生的结构颜色之间的直接关系.
结论:
- 阿莫莱特的独特,生动的结构颜色主要是由于化石内间层纳米间隙的特定光反射.
- 这些纳米间隙,它们的一致的层化周期和厚度依赖性质,对于观察到的干扰现象和充满活力的色彩至关重要.
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