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Constructed wetlands (CWs) treating nitrate-rich wastewater often face incomplete denitrification and elevated NO emissions due to insufficient electron donors. Pyrrhotite as a CW substrate demonstrated potential for enhancing autotrophic denitrification through coupled sulfur and iron biological oxidation. However, the impact of pyrrhotite layer positioning on regulating NO emissions and underlying mechanisms remains unclear. This study evaluated the effect of pyrrhotite layer placement (top, middle and bottom) on S/Fe-coupled denitrification and NO release under organic carbon-free with varying nitrogen loads. Results showed that the bottom layer achieved 32.36-65.86 % complete denitrification (2.37-5.68 times higher than middle/top layers), while B-CW limited NO emission to only 0.36 % of converted nitrate (39.60-53.60 % lower than M-CW/T-CW). Enhanced performance in B-CW correlated with higher oxidation amounts of reduced sulfur (50.51 vs. 25.27-28.97 mg/L) and ferrous iron (36.83 vs. 18.43-21.12 mg/L), with efficient utilization. Network analysis revealed increased modularity and functional clustering in the bottom layer, with Ralstonia co-occurring with key sulfur/iron-cycling bacteria (Thiobacillus, Undibacterium) to form stable denitrifying consortia. Microbial analysis revealed enrichment of nitrate-reducing bacteria, primarily Ralstonia (14.69 %) in the bottom layer, driving 66.58 % inorganic electron utilization via sulfur oxidation-coupled complete denitrification. Electron and nitrogen mass balances revealed that 81.84 % of reduced nitrate was converted to N Additionally, synergistic interactions among nitrate-reducing bacteria (24.19 %), sulfur-/iron-oxidizing bacteria (16.29 %/4.46 %), organic matter-degrading bacteria (23.23 %), and electroactive bacteria (8.12 %) supported the process. These findings highlight pyrrhotite layer depth as a critical regulator of NO mitigation in CWs, providing a sustainable inorganic strategy for low-carbon and sustainable nitrogen removal.
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http://dx.doi.org/10.1016/j.biortech.2025.133295 | DOI Listing |
Bioresour Technol
September 2025
Research Division for Water Environmental Science and Engineering, Institute of Hydrobiology, Chinese Academy of Sciences, Wuhan 430072, China. Electronic address:
Constructed wetlands (CWs) treating nitrate-rich wastewater often face incomplete denitrification and elevated NO emissions due to insufficient electron donors. Pyrrhotite as a CW substrate demonstrated potential for enhancing autotrophic denitrification through coupled sulfur and iron biological oxidation. However, the impact of pyrrhotite layer positioning on regulating NO emissions and underlying mechanisms remains unclear.
View Article and Find Full Text PDFJ Environ Sci (China)
November 2025
Institute of Water Ecology and Environment, Chinese Research Academy of Environmental Sciences, Beijing 100012, China. Electronic address:
Pyrrhotite oxidation poses a big threat to water environment duo to its high potential for generating pollutants. Hydrogen peroxide, commonly found in natural water at micromolar concentrations, possesses much more aggressive oxidation ability than oxygen and can complicate the pyrrhotite oxidation process. Here, the effects of micromolar HO on the biotic and abiotic oxidation of pyrrhotite were examined at pH 1.
View Article and Find Full Text PDFJ Phys Chem C Nanomater Interfaces
March 2025
Dpto. de Física de Materiales, Facultad de Ciencias, Universidad Autónoma de Madrid, Francisco Tomás y Valiente 7, E-28049 Madrid, Spain.
This work presents a comprehensive reaction and kinetic model of the pyrite thin films formation by sulfuration of Fe monosulfides when a molecular sulfur (S) atmosphere is used. This investigation completes the results already published on the explanation and interpretation of the sulfuration process that transforms metallic iron into pyrite. It was previously shown that the monosulfide species (i.
View Article and Find Full Text PDFMiner Depos
July 2023
DEL Exploration, Paradise, Paradise, NL A1L 1V6 Canada.
Unlabelled: The Current deposit is hosted by serpentinized peridotite that intruded rocks of the Quetico Subprovince in the Midcontinent Rift, and is subdivided into three morphologically distinct regions - the shallow and thin Current-Bridge Zone in the northwest, the deep and thick 437-Southeast Anomaly (SEA) Zone in the southeast, and the thick Beaver-Cloud Zone in the middle. The magma parental to the Current deposit became saturated in sulfide as a result of the addition of external S from at least two sources - a deep source characterized by high ΔS (< 3‰) values, and a shallow source, potentially the Archean metasedimentary country rocks, characterized by low ΔS (< 0.3‰).
View Article and Find Full Text PDFNanoscale Adv
August 2023
Institute of Atomic and Molecular Sciences, Academia Sinica Taipei Taiwan
Conventional exfoliation exploits the anisotropy in bonding or compositional character to delaminate 2D materials with large lateral size and atomic thickness. This approach, however, limits the choice to layered host crystals with a specific composition. Here, we demonstrate the exfoliation of a crystal along planes of ordered vacancies as a novel route toward previously unattainable 2D crystal structures.
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