在热水条件下,非生态甲的形成和同位素分离
1Chemical and Analytical Sciences Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831, USA. Department of Geology and Geophysics, University of Minnesota, Minneapolis, MN 55455, USA.
概括
在热水条件下,非生态甲形成由铁合金催化. 这一过程产生了与微生物甲相似的同位素特征的甲 (CH4),这表明可能存在广泛的无源甲.
科学领域:
- 地质化学 地质化学
- 生物地质化学生物地质化学
- 矿物学是什么?矿物学是什么?
背景情况:
- 在地球地中越来越多地发现潜在的生物起源的甲 (CH4).
- 生物甲形成的机制和同位素分离仍然不太清楚.
研究的目的:
- 为了研究水热铁合金在非生态甲形成中的催化作用.
- 为了分析在这种非生态甲合成过程中的同位素分离.
主要方法:
- 使用铁合金催化剂实验模拟热水条件.
- 溶解的二碳酸盐 (HCO3-) 与催化剂的反应形成甲 (CH4).
- 对产生的甲和相关碳化合物的同位素分析 (delta(13) C).
主要成果:
- 在水热条件下,铁合金有效地催化了从二碳酸盐 (HCO3-) 形成非生态甲 (CH4).
- 同位素分离导致CH4的低值,与微生物甲相美.
- 观察到高的CH4 / ((C2H6 + C3H8) 比率,模仿生物生产.
结论:
- 水热-铁合金可以催化具有生物学相关同位素特征的无源甲形成.
- 在海洋地中铁合金的普遍存在表明,这是一个显著的,以前被低估的非生态甲来源.
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