前坎布里亚大陆石化层对全球H2生产的贡献
Barbara Sherwood Lollar1, T C Onstott2, G Lacrampe-Couloume1
1Department of Earth Sciences, 22 Russell Street, University of Toronto, Toronto M5S 3B1, Canada.
Nature
|December 19, 2014
概括
全球从前坎布里亚岩石生产的气 (H2) 产量被大大低估. 新的数据显示,H2的生产速度与海洋系统相比,影响了我们对地下微生物生态系统的理解.
科学领域:
- 地质化学 地质化学
- 微生物学 微生物学
- 地下科学 地下科学
背景情况:
- 微生物生态系统依赖于来自水岩相互作用的气 (H2).
- 海洋石质层H2产量估计为每年10~11个摩尔.
- 前坎布里亚时代地下H2水平与水热通风口相竞争,与水放射溶解有关.
研究的目的:
- 重新评估前坎布里亚大陆石化层的H2生产潜力.
- 为了解决这些环境中低估的H2流量问题.
- 为了比较大陆石质层的H2产量与海洋系统.
主要方法:
- 全球编已公布和新的H2度数据从前坎布里亚岩石.
- 包括从蛇形化和放射溶解中产生H2的情况.
- 对H2测量的缩放,考虑了前坎布里亚时期的地表面积.
主要成果:
- 预坎布里亚大陆石化层的H2生产潜力被低估了.
- 据估计,H2的生产率为每年0.362.27 × 10(11) 摩尔.
- 这一速度相当于海洋系统中的H2产量.
结论:
- 在前坎布里亚大陆石化层中,H2的产生是显著的.
- 放射溶解和水合反应是主要的H2来源.
- 地下微生物生态系统可能比以前认为的更广泛.
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