Effect of organic matter derived from algae and macrophyte on anaerobic ammonium oxidation coupled to ferric iron reduction in the sediment of a shallow freshwater lake

Effect of organic matter derived from algae and macrophyte on anaerobic ammonium oxidation coupled to ferric iron reduction in the sediment of a shallow freshwater lake
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来自藻类和水生植物的有机物对浅淡水湖沉积物中厌氧铵氧化与三价铁还原的影响

DOI:
10.1007/s11356-019-06793-5
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发表时间:
2019-11
影响因子:
5.8
通讯作者:
Helong Jiang
Helong Jiang
中科院分区:
环境科学与生态学3区
文献类型:
--
作者:
Zongbao Yao;Liu Yang;Na Song;Changhui Wang;Helong Jiang

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作为一种近期发现的氮循环过程,厌氧氨氧化与三价铁还原耦合(Feammox)受到了更多关注。本研究调查了一个……(句子不完整,最后一个单词“a s”可能有误)不同区域沉积物中Feammox的空间变化。
As a recently discovered process of nitrogen cycling, anaerobic ammonium oxidation coupled to ferric iron reduction (Feammox) has attracted more attentions. This study investigated the spatial variation of Feammox in the sediment of different zones of a shallow freshwater lake and the effect of organic matter derived from algae and macrophyte on Feammox process. The potential Feammox rates showed significant differences among sediments from algae-dominated area (ADA), transitional area in the center of the lake (TDA), and macrophyte-dominated area (MDA), and in a descending order, ADA, MDA, and TDA. The potential Feammox rate ranged from 0.14 to 0.34 mg N kg−1day−1in the freshwater lake sediment. The potential Feammox rates of the sediment with algae or macrophyte amendment were 12.29% and 15.31% higher than the control test without algae and macrophyte amendment. The addition of algae or macrophyte to the sediment from TDA could improve the amount of HCl-extractable total Fe, Fe(III) reduction rate, and the abundance of FeRB. These results demonstrated that organic matter is one of the key regulators of Feammox process.
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