有效地限制由富含铁的红土在Ulva繁殖丰富的海洋沉积物中产生的溶解硫化物
Yang-Yang Guo1, Tie Li1, Xiao-Yan Cao1
1Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China.
Marine pollution bulletin
|May 1, 2024
概括
富含铁的红色土壤有效地缓冲了来自宏藻繁殖的溶解硫化物 (DS). 在藻类沉积之前和之后应用红色土壤会限制DS,防止积累和减轻海底影响.
科学领域:
- 海洋化学 海洋化学
- 环境科学环境科学
- 地质化学 地质化学
背景情况:
- 宏观藻类的开花通过硫酸盐还原导致溶解硫化物 (DS) 积累.
- 沉积铁 (Fe) 与DS反应,但往往无法防止脉冲开花的积累.
研究的目的:
- 评估富含铁的红土在缓冲大藻丰富沉积物中DS的有效性.
- 为了评估红色土壤的长期缓冲能力.
主要方法:
- 使用大藻 (Ulva prolifera) 丰富沉积物的化实验.
- 在模拟宏藻沉积之前和之后,应用富含铁的红土.
主要成果:
- 红色土壤添加剂 (6.8 kg/m2) 有效地在土壤层内限制了DS.
- 红色土壤中充足的氧化铁表面区域促进了DS反应和缓冲.
- 在18天后,缓冲能力的最小损失 (4%) 表明了持续的性能.
结论:
- 富含铁的红土是一种有希望的材料,可以减轻巨藻繁殖造成的DS污染.
- 预存和后存款上限的应用策略是有效的.
- 红土在受影响的海洋沉积物中提供长期的DS缓冲.
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