概括
钻石漂浮在原始地幔中,在高压下融化,这表明过渡区可能是一个重要的钻石储存库. 这一发现影响了我们对地球的理解.
科学领域:
- 地质化学 地质化学
- 矿物物理 矿物物理
- 高压实验科学 高压实验科学
背景情况:
- 了解地球深层内部碳相的行为对于破译地幔过程至关重要.
- 以前的钻石在地幔中的稳定性和运输模型一直受到直接实验数据的限制.
研究的目的:
- 为了实验性地确定与原始地幔相对的钻石密度,在高压和高温下化.
- 调查钻石浮力对其在地球过渡区积累的影响.
主要方法:
- 高压,高温钻石杆细胞实验.
- 在合成的地幔融成分中观察钻石的行为 (浮动或沉降).
- 精确测量压力和温度条件.
主要成果:
- 观察到钻石在原始地幔融化中漂浮,温度约为20千兆帕斯卡尔和2360摄氏度.
- 钻石也漂浮在一个来自过渡区的融中,温度约为16千兆帕斯卡尔和2270摄氏度.
- 这些结果为深层地幔条件下的岩密度提供了直接的约束.
结论:
- 钻石在深层地幔融化的浮力表明,它可以在过渡区积聚.
- 过渡区可能是从地球早期历史以来长期沉或被困钻石的储存库.
- 这种积累机制对深层碳循环和地幔演变有重大影响.
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