概括
在酸性湖泊孔水中溶解的形成不溶性硫化物,导致沉积在沉积物中. 地表下峰可能表明了代遗传过程,而不仅仅是湖泊酸化.
科学领域:
- 环境化学环境化学
- 地质化学 地质化学
- 临界技术 临界技术
背景情况:
- 酸性湖泊在水和无氧孔水之间呈现的溶解梯度.
- 无氧孔水中的低度表明不溶性硫化矿物质的形成.
研究的目的:
- 为了研究在酸性湖泊沉积物中溶解的的命运.
- 为了确定向下扩散流对沉积的贡献.
- 探索湖泊沉积物中地下最大值的原因.
主要方法:
- 在上层水和无氧孔水中分析溶解的度.
- 量化溶解的向下扩散流.
- 观测沉积体内总分布的情况.
主要成果:
- 溶解的向下扩散流为最近的沉积贡献了50-75%.
- 在沉积物-水界面下2-3厘米观察到总的明显地表下最大值.
- 这些地下峰可能是由于与最近的湖泊酸化无关的基因活动引起的.
结论:
- 硫化沉是控制无氧孔水中的度的关键过程.
- 独立于最近的酸性化过程,可在湖泊沉积物中产生地下峰.
- 了解代谢对于解释酸性湖中的沉积物记录至关重要.
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