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燃烧和 Pyrolysis EA-IRMS 技术来确定钻石的 H
François Fourel1, Christophe Lécuyer2, Emilie Thomassot3
1Laboratoire d'Ecologie des Hydrosystèmes Naturels et Anthropisés LEHNA UMR CNRS 5023, Université Claude Bernard Lyon 1, 3 rue Raphaël Dubois - Bât. Forel, Villeurbanne Cedex, France.
研究人员开发并验证了测量钻石中同位素的新方法. 这种技术为地球提供了至关重要的洞察力.
科学领域:
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
- 同位素分析分析 同位素分析
背景情况:
- 钻石起源于地球的地幔,由碳含量流体与深层石质学相互作用而形成.
- 研究矿物质含量和稳定的同位素揭示了钻石形成过程.
- 钻石为地球地幔的挥发性元素组成提供了独特的见解,包括杂质.
研究的目的:
- 开发和验证用于量化天然钻石中气度和同位素组成的新型分析技术.
- 建立可靠的方法对碳,氧和在钻石中的同位素分析.
- 提高对天然钻石形成过程和深水循环的理解.
主要方法:
- 两种涉及元素分析仪-同位素比质谱法 (EA-IRMS) 的技术的比较.
- 第一种方法:改性H-热解.
- 第二种方法:新型钻石燃烧,然后减少.
主要成果:
- 使用石墨和多晶钻石样本验证两个EA-IRMS技术.
- 从H-热解和钻石燃烧方法中获得的高度可比的结果.
- 证实H-热解方法的有效性和稍高的灵敏度.
结论:
- 设计和验证了一种用于钻石中同位素分析 (碳,氧,和) 的新方法.
- 使用这种技术进行现场钻石分析可以提高对地球深层水循环的理解.
- 开发的方法可以提供精确校准的材料,这对于准确的同位素测量至关重要.
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