相关实验视频
Updated: Jul 12, 2026

05:39
Shock Wave Application to Cell Cultures
Published on: April 8, 2014
概括
冲击石英可以转化为stishovite,一个高压的二氧化多态. 这项研究在冲击砂岩和石英中发现了石灰岩,这表明在极端压力和温度条件下存在新的转化途径.
科学领域:
- 地质地质地质地质地质地
- 矿物学是什么?矿物学是什么?
- 冲击物理 冲击物理
背景情况:
- 斯蒂索维特是二氧化的高压多态.
- 以前的研究表明,coesite是冲击石英的常见产物.
研究的目的:
- 为了研究在爆炸性冲击后的石英含岩石中石灰岩的形成.
- 了解石英在冲击条件下的转变机制.
主要方法:
- 对爆炸性冲击的砂岩,新岩和单晶石英的分析.
- 使用显微镜和潜在的其他分析技术分离和识别stishovite.
- 估计高峰冲击压力 (150-280 kbar) 和温度 (150-900°C).
主要成果:
- 从受冲击的标本中成功分离出了少量的stishovite.
- 在任何分析的样本中都没有检测到coesite.
- 峰值压力在150至280千巴之间,冲击温度在150°C至900°C之间.
结论:
- 石英可以在冲击下逆转为短距离顺序,六个协调相.
- 这一阶段可以转化为stishovite.
- 在特定条件下,例如在石撞击期间,这个阶段也可能逆转为coesite.
相关概念视频
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Protons and neutrons, collectively called nucleons, are packed together tightly in a nucleus. With a radius of about 10−15 meters, a nucleus is quite small compared to the radius of the entire atom, which is about 10−10 meters. Nuclei are extremely dense compared to bulk matter, averaging 1.8 × 1014 grams per cubic centimeter. If the earth’s density were equal to the average nuclear density, the earth’s radius would be only about 200 meters.
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