在石中含有四价
1N. C. Sturchio, M. R. Antonio, L. Soderholm, Argonne National Laboratory, Argonne, IL 60439, USA. S. R. Sutton, Consortium for Advanced Radiation Sources and Department of Geophysical Sciences, University of Chicago, Chicago, IL 60637, USA.
四价稳定地替代了在减少环境中形成的古老石中的. 这一发现支持系列测定石的年龄,并突出了其在地下水和盆地中封存中的作用.
科学领域:
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
- 射线测量约会的方法
背景情况:
- 石是一种常见的矿物质,可以包含各种元素.
- 系列测年依赖于可预测的同位素的衰变.
- 了解在地质构成中的行为对于约会准确性和环境研究至关重要.
研究的目的:
- 为了研究在古代石中的替代.
- 在特定条件下,在石中确定的稳定性和价值状态.
- 评估对系列测年方法和封存的影响.
主要方法:
- 射线吸收光谱 (XAS) 用于确定的化学状态.
- 进行X射线光微探测器 (XFM) 分析,绘制分布图.
- 从密西西比河谷类型的沉积物中研究了3500万年前的石.
主要成果:
- 有证据表明,四价 (U4+) 在石中取代双价 (Ca2+).
- 证实四价在减少条件下形成的酸盐中稳定.
- 鉴定石作为无氧环境中的重要沉积点.
结论:
- 替代机制验证了古老的石的系列约会 (例如,/约会).
- 石作为天然的陷在深地下水,无氧湖水和海洋盆地.
- 这项研究提高了我们对地球化学过程和放射测年技术的理解.
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