来自北极环保湖浅区域的高内部负荷:来自孔水地质化学的洞察力
Siqi Zhao1, Martijn Hermans2, Juha Niemistö3
1Ecosystems and Environment Research Program, Faculty of Biological and Environmental Sciences, University of Helsinki, Viikinkaari 1, P.O. Box 65, FI-00014 Helsinki, Finland; Environmental Geochemistry Group, Department of Geosciences and Geography, Faculty of Science, University of Helsinki, Gustaf Hällströmin katu 2, P.O. Box 64, FI-00014 Helsinki, Finland.
The Science of the total environment
|October 21, 2023
概括
内部加载燃料湖的环氧化. 在富含铁的湖泊中,有机物再矿化和铁结合溶解驱动P释放,即使在氧气条件下,也会影响湖泊的恢复.
科学领域:
- 环境化学环境化学
- 临界技术 临界技术
- 地质化学 地质化学
背景情况:
- 内部 (P) 负载是湖泊缩的关键驱动因素.
- 铁 (Fe) 氧化物在氧化条件下限制P扩散的作用受到辩论.
- 了解性,富含铁的沉积物中的P动态至关重要.
研究的目的:
- 在两个富含铁的芬兰湖泊中研究沉积物P循环.
- 评估有机物 (OM) 重矿化和与Fe结合的P (Fe-P) 溶解对P再生的影响.
- 为了评估控制P释放到水柱中的因素.
主要方法:
- 对孔水和固态样本的分析.
- 评估控制沉积物P循环的基因过程.
- 在Hiidenvesi湖和Kytäjärvi湖的生物地化学P动态的调查.
主要成果:
- 结合Fe-P溶解和OM重矿化控制P再生,以Fe-P为主要来源.
- 在深层沉积物中,vivianite形成可能会使P固定不动.
- 由于在更高的温度下增强OM重矿化,在浅,有氧位点发生了升高的P扩散.
- 氧气区域全年显示出比无氧/低氧区域更高的盆地P流量.
结论:
- 富含铁的温湖中的沉积物P循环是复杂的,受OM重矿化和Fe-P动态的影响.
- 即使在浅,温暖,富含OM的沉积物中,高Fe/P比率也可能发生显著的P释放.
- 这些发现对管理内部P负载和湖泊恢复策略有影响.
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