厌氧氨氧化菌
硝酸盐
化学
电子转移
反硝化
黄铁矿
硫化物
铵
环境化学
氮气
硝酸还原酶
氮气循环
无机化学
化学工程
矿物学
有机化学
工程类
反硝化细菌
作者
Fan Feng,Zhigong Liu,Xi Tang,Xing Wu,Caiyan Qu,Seow Wah How,Di Wu,Ruiyang Xiao,Chong-Jian Tang,Zhang Lin,Liyuan Chai,Guanghao Chen
出处
期刊:Water Research
[Elsevier BV]
日期:2022-11-20
卷期号:229: 119393-119393
被引量:126
标识
DOI:10.1016/j.watres.2022.119393
摘要
Anaerobic ammonium oxidation (anammox) represents an energy-efficient process for biological nitrogen removal from ammonium-rich wastewater. However, there are mechanistic issues unsolved regarding the low microbial electron transfer and undesired accumulation of nitrate in treated water, limiting its widespread engineering applications. We found that the addition of pyrite (1 g L-1 reactor), an earth-abundant iron-bearing sulfide mineral, to the anammox system significantly improved the nitrogen removal rate by 52% in long-term operation at a high substrate shock loading (3.86 kg N m-3 d-1). Two lines of evidence were presented to unravel the underlying mechanisms of the pyrite-induced enhancement. Physiochemical evidence indicated that an increase of cytochromes c and Fe-S protein was responsible for the accelerated electron transfer among metabolic enzymes. Multi-omics evidence showed that the depletion of nitrate was attributed to the Fe-N-S cycle driven by nitrate-dependent Fe(II) oxidation and S-based denitrification. This study deepens our understanding of the roles of electron transfer and the Fe-N-S cycle in anammox systems, providing a fundamental basis for the development of mediators in the anammox process for practical implications.
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