丰富的孔水Mn(III) 是沉积物的氧化还原系统的主要组成部分
Andrew S Madison1, Bradley M Tebo, Alfonso Mucci
1School of Marine Science and Policy, University of Delaware, Lewes, DE 19958, USA. andrew_madison@golder.com
概括
溶性 (III) 是沉积物中循环的一个主要,被忽视的组成部分. 这项研究揭示了它在接近表面的孔水中的重要作用,影响了氧化还原反应.
科学领域:
- 地质化学 地质化学
- 环境科学 环境科学
- 海洋化学 海洋化学
背景情况:
- 溶性 ((III) [Mn ((III) ]在氧化还原反应中充当氧化剂和还原剂.
- 尽管在循环中具有潜在的意义,但在近地表沉积物孔水中经常被忽视.
研究的目的:
- 调查在半沉积物中可溶性的作用和丰度.
- 了解沉积环境中可溶性的形成途径.
主要方法:
- 采用了一种光谱光度运动方法.
- 分析是在加拿大北克省劳伦斯河谷的半沉积物上进行的.
- 研究了溶解氧,溶解和固体的垂直形状.
主要成果:
- 溶性,稳定由连接物,构成高达90%的总溶解池.
- 溶性 (Mn) 主要是由向上扩散的无氧沉积物中产生的 (Mn) 氧化.
- 对溶性的较小贡献来源于MnO2的还原性溶解.
结论:
- 溶性 (III) 是沉积循环的关键,被低估的组成部分.
- 沉积式氧化还原循环的概念模型必须包含溶解的.
- 连接物稳定是孔水中可溶Mn (III) 的存在的关键.
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