吸附和共沉降二碳酸盐与铁酸盐的独特光化学:对铁的还原性溶解和碳稳定性的影响
Qingchao Li1, Yu Fu1, Lingli Wang1
1Shanghai Key Lab for Urban Ecological Processes and Eco-Restoration, School of Ecological and Environmental Sciences, East China Normal University, Shanghai 200241, China.
The Science of the total environment
|April 12, 2024
概括
铁 (FH) 与有机酸 (LMWOAs) 的光溶解取决于它们如何结合. 与吸附的LMWOA相比,共同沉积的FH-LMWOA显示出不同的光化学反应,影响铁氧化还原循环.
科学领域:
- 环境地质化学环境地质化学
- 摄影化学的使用
- 矿物学是什么?矿物学是什么?
背景情况:
- 已知通过低分子量有机酸 (LMWOAs) 促进化 (FH) 的联体光溶解.
- 共同沉的FH-LMWOAs协会的光化学仍然不太了解,尽管它们在碳保留中的重要性很重要.
- 了解这些关联对于矿物有机界面的铁氧化还原循环至关重要.
研究的目的:
- 为了研究铁酸盐-LMWOAs协会 (FLAs) 的光溶解动力学.
- 在FH和溶解Fe-LMWOAs复合体上比较共沉积的FLA与吸附的LMWOAs的光化学.
- 阐明LMWOA的关联模式和配置对FH光反活性的作用.
主要方法:
- 在环中性条件下合成FLA.
- 监测Fe(II) 的形成和有机碳衰变,以评估光溶解动力学.
- 描述LMWOAs的关联模式 (吸附与共降) 和FH上的配置.
主要成果:
- 在水性复合物中的Fe (II) 产量取决于LMWOA度和基质性质.
- 吸附的FH-oxalate的内部球单核双形态配置具有高度的光反应性.
- 共同沉的FLAs显示出增强的Fe(II) 产量,具有较高的LMWOA含量,与中度含量不同,由于各种联结模式和连接物可用性.
结论:
- 协会的模式 (吸附与共降) 和LMWOAs的配置显著影响FH光化学.
- 共同沉引入了与表面吸附一起的内部包含,改变了光反活性.
- 这些发现凸显了矿物有机联体中铁氧化还原循环的复杂性.
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