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微生物氧化显著减少了全球地下水中的甲出口.

Beatrix M Heinze1,2, Valérie F Schwab1, Kirsten Küsel2,3,4

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微生物氧化显著减少地下水中甲的释放. 这项研究量化了甲氧化率,揭示了地下水微生物群作为重要的甲过器,减轻了环境问题.

关键词:
测量14C-率的测量地下水 地下水 地下水微生物甲氧化的过程

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科学领域:

  • 环境科学 环境科学
  • 微生物学 微生物学
  • 地质化学 地质化学

背景情况:

  • 地下水中的甲是越来越严重的环境问题,因为它被释放到地表环境中.
  • 微生物氧化是甲消耗的关键过程,但其在地下水中的速度尚不清楚.

研究的目的:

  • 在德国含水层中量化微生物甲氧化率在广泛的甲度范围内.
  • 为了确定参与甲氧化中的微生物群落.
  • 为了估计地下水甲氧化对甲释放的全球影响.

主要方法:

  • 超低级C标签用于测量甲氧化速率.
  • 对五个数量级的甲度进行分析.
  • 微生物社区分析以确定主导的甲类植物.

主要成果:

  • 甲氧化率与甲度有很强的相关性,范围从0.001到74.28μgC L-1 d-1.
  • 甲循环时间在低度下从几天到几周,在高度下从几个月到几十年不等.
  • 特定的微生物群体,包括马蛋白细菌和无氧甲氧化古生物,与高氧化率有关.

结论:

  • 地下水微生物群作为一个关键的甲过器,去除全球约66%的地下水甲 (167778 Tg CH4-1).
  • 高度的甲可能导致不完全的氧化,增加甲释放的可能性.
  • 了解这些微生物过程对于预测地下水中的甲流量至关重要.