概括
溶解的氧气随着太平洋沉积物深度的下降而减少,由于生物化有限的有机碳供应而平衡. 这会在沉积物-水界面上产生可测量的氧气梯度和扩散流.
科学领域:
- 海洋地质学 海洋地质学
- 地质化学 地质化学
- 海洋学 海洋学 海洋学
背景情况:
- 研究了赤道太平洋中部的沉积物,特别是海底红色粘土和碳酸.
- 了解海洋沉积物中的氧气动态对于生物地球化学循环至关重要.
研究的目的:
- 为了研究海洋沉积物中溶解氧的垂直分布.
- 为了确定控制深度氧气消耗的因素.
- 量化通过沉积物-水界面的扩散氧气流.
主要方法:
- 在海洋沉积物的间歇水中溶解氧的现场测量.
- 对沉积物组成的分析 (红色粘土,碳酸).
- 通过生物化对有机碳供应的评估.
主要成果:
- 溶解氧含量随着沉积物深度的增加而减少.
- 在较深的水平上,氧气度稳定在非零值.
- 受生物流影响的活性有机碳供应限制了氧气消耗.
- 通过沉积物-水接口计算的平均扩散氧气流量为8.8 x 10(-14) mol/cm2/s.
结论:
- 生物流在深海沉积物中调节氧气消耗方面发挥着关键作用.
- 观察到的氧气梯度驱动可测量的扩散氧气流.
- 沉积物地质化学和物理过程显著影响盆地氧气动态.
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