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西西伯利亚的甲陆地透:起源,运输和生产的代谢途径
Aleksandr F Sabrekov1,2, Irina E Terentieva3, Gregory J McDermid3
1UNESCO Department "Environmental Dynamics and Global Climate Changes", Ugra State University, Khanty-Mansiysk, Russia.
Global change biology
|July 6, 2023
概括
西西伯利亚的甲入来源于泥炭地,而不是深层石油或永久土. 地下水在运输这种甲方面发挥着关键作用,突出显示了它在北极-泰加生物群中的重要性.
科学领域:
- 地质化学 地质化学
- 环境科学 环境科学
- 地质地质地质地质地质地
背景情况:
- 西西伯利亚的泥炭地储存了大量的碳,覆盖着一个主要的碳化合物盆地.
- 在西西伯利亚平原的大片地区发现了陆地甲泄漏.
研究的目的:
- 确定西西伯利亚陆地漏中甲的起源和迁移途径.
- 测试涉及深层石油储备,退化永久土和泥炭地来源的假设.
主要方法:
- 来自漏,泥炭地和含水层的气体和水样的分析.
- 使用地质化学工具,包括放射性碳年代和稳定同位素分析.
主要成果:
- 甲成分,年龄和同位素数据强烈支持泥炭地起源 (H3).
- 甲通过二氧化碳减排在沼泽中产生,通过乙生成和乙酸发酵在地下水中产生.
- 通过地下水连接的横向迁移对于甲运输至关重要.
结论:
- 泥炭地是西西伯利亚入的甲的主要来源.
- 地下水促进甲迁移,使河流和泉水成为潜在的甲来源.
- 这一过程在全球类似的泥炭地丰富的景观中可能具有重要意义.
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