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Denitrification and Anammox and Feammox in the Yinchuan Yellow River wetland

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  • Qingsong Guan

    (Breeding Base for State Key Laboratory of Land Degradation and Ecological Restoration in Northwestern China; Key Laboratory of Restoration and Reconstruction of Degraded Ecosystems in Northwestern China of Ministry of Education, Ningxia University, Yinchuan, P.R. China
    College of Application of Engineering, Henan University of Science and Technology, Sanmenxia, P.R. China
    Engineering Technology Research Center of Sanmenxia Yellow River Wetland Environmental Process and Ecological Restoration, Sanmenxia, P.R. China)

  • Yiqiao Zhou

    (College of Application of Engineering, Henan University of Science and Technology, Sanmenxia, P.R. China
    Engineering Technology Research Center of Sanmenxia Yellow River Wetland Environmental Process and Ecological Restoration, Sanmenxia, P.R. China)

  • Shuo Li

    (College of Application of Engineering, Henan University of Science and Technology, Sanmenxia, P.R. China
    Engineering Technology Research Center of Sanmenxia Yellow River Wetland Environmental Process and Ecological Restoration, Sanmenxia, P.R. China)

  • Fan Yang

    (College of Application of Engineering, Henan University of Science and Technology, Sanmenxia, P.R. China
    Engineering Technology Research Center of Sanmenxia Yellow River Wetland Environmental Process and Ecological Restoration, Sanmenxia, P.R. China)

  • Rentao Liu

    (Breeding Base for State Key Laboratory of Land Degradation and Ecological Restoration in Northwestern China; Key Laboratory of Restoration and Reconstruction of Degraded Ecosystems in Northwestern China of Ministry of Education, Ningxia University, Yinchuan, P.R. China)

Abstract

Denitrification, anaerobic ammonium oxidation (Anammox), and ferric iron reduction coupled with anaerobic ammonium oxidation (Feammox) are the nitrogen removal pathways in natural ecosystems. In this study, the differences between these three nitrogen removal pathways in a Phragmites australis covered site (LW), artificial grassland covered site (CD), poplar covered site (YD), and topsoil tillage after harvesting reed site (GD) in the Yinchuan Yellow River wetland were investigated using isotope tracing, metagenome, and quantitative polymerase chain reaction (Q-PCR) techniques. No 30N2 accumulation was detected in 15NH4+ addition incubations, indicating that Feammox was weak in all sites, which is consistent with a low abundance of the Feammox functional bacteria Acidimiprobiaceae sp. A6. The denitrification rates were 0.36 (LW), 0.5 (CD), 0.76 (YD) and 0.12 (GD) mg N/kg/day. The Anammox rates were 0.18 (LW) and 0.26 (GD) mg N/kg/day; other sites did not detect Anammox rate. Denitrification was the dominant pathway except for the CD site. The YD site had the highest abundance of denitrification genes, which was consistent with the denitrification rate.

Suggested Citation

  • Qingsong Guan & Yiqiao Zhou & Shuo Li & Fan Yang & Rentao Liu, 2024. "Denitrification and Anammox and Feammox in the Yinchuan Yellow River wetland," Plant, Soil and Environment, Czech Academy of Agricultural Sciences, vol. 70(11), pages 731-738.
    • Handle: RePEc:caa:jnlpse:v:70:y:2024:i:11:id:318-2024-pse
    DOI: 10.17221/318/2024-PSE
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    References listed on IDEAS

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    1. Nicolas Gruber & James N. Galloway, 2008. "An Earth-system perspective of the global nitrogen cycle," Nature, Nature, vol. 451(7176), pages 293-296, January.
    2. Tage Dalsgaard & Donald E. Canfield & Jan Petersen & Bo Thamdrup & Jenaro Acuña-González, 2003. "N2 production by the anammox reaction in the anoxic water column of Golfo Dulce, Costa Rica," Nature, Nature, vol. 422(6932), pages 606-608, April.
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