概括
基伍湖拥有巨大的甲储量. 最近的数据表明,这种深水甲的主要来源是细菌过程,而不是火山活动或有机衰变.
科学领域:
- 地质化学 地质化学
- 微生物学 微生物学
- 临界技术 临界技术
背景情况:
- 基伍湖 (Kivu湖) 是非洲的一个裂湖,它含有约50立方公里的甲 (在标准温度和压力下) 在深水中溶解.
- 这种大量甲储量的起源一直是科学调查的主题,以前考虑过火山和有机分解假设.
研究的目的:
- 为了调查基伍湖甲的来源.
- 区分生物遗传,火山和有机的甲来源.
主要方法:
- 分析了最近两次前往基伍湖的探险队的数据.
- 重新评估之前收集的湖泊数据.
主要成果:
- 有证据表明,基伍湖中的大部分甲是通过生物遗传过程产生的.
- 具体来说,细菌对二氧化碳和的转化似乎是主要的甲形成途径.
- 火山活动或有机物分解对甲库的贡献很可能是最小的.
结论:
- 基伍湖中的甲主要是生物遗传的,是由微生物活动形成的.
- 这一发现对了解大型无毒湖中的甲循环有着重大意义.
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