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Homoacetogenesis inhibition and electrode regulation strengthen an in situ hydrogen-retaining reducing environment for Fe3+ reduction-driven vivianite formation

  • Zhengtong Guo
  • , Xianbao Xu
  • , Zhihong Liu*
  • , Jinying Wang
  • , Yuan Li
  • , Bogna Śniatała
  • , Benyamin Chahkandi
  • , Wenzong Liu
  • , Xiuping Yue
  • , Aijuan Zhou
  • , Francisco Jesús Fernández-Morales
  • , Jacek Mąkinia
  • *Corresponding author for this work
  • Taiyuan University of Technology
  • Gdańsk University of Technology
  • Shanghai University of Engineering Science
  • Harbin Institute of Technology Shenzhen
  • University of Castilla-La Mancha

Research output: Contribution to journalArticlepeer-review

Abstract

Vivianite, a valuable secondary Fe-P mineral, recovery from waste activated sludge provides a promising strategy for sustainable phosphorus (P) recovery and value-added utilization. However, competitive H2 consumption by homoacetogenesis and the insufficient reducing environment for Fe3+ reduction limit the vivianite formation. This study introduces chloroform (0.02% (v/v)) to suppress homoacetogenesis and further optimizes iron anode voltage to improve H2 retention, electron transfer, and Fe-P mineralization. Chloroform addition improved Fe2+ utilization efficiency, while further synergistic regulation of iron anode voltage increased Fe2+ utilization efficiency to 70.5%, and both contributed to improving vivianite quality. In particular, the chloroform-operated at 0.6 V (C-0.6 V) series achieved the highest vivianite size, crystallinity, and purity of 89.3 μm, 95.8%, and 94.7%, respectively. Chloroform reduced acetate accumulation, and the relative abundance of homo-acetogens decreased from 51.1% in the 0.8 V without chloroform (Control-0.8 V) series to 15.8% in the chloroform-operated at 0.8 V (C-0.8 V) series, whereas C-0.6 V further enriched electroactive bacteria (EAB) and dissimilatory iron-reducing bacteria (DIRB), indicating a shift of electron flow from competitive H2 consumption toward Fe3+ reduction processes. Meanwhile, 0.6 V provided a favorable electrochemical window, strengthening Fe3+ reduction-related electron transfer pathways, and then promoted efficient electron delivery from intracellular metabolism to extracellular Fe3+ acceptors. Chloroform reshaped electron allocation by suppressing homoacetogenesis, while the optimized iron anode voltage strengthened the coupling between Fe3+ reduction and electron transfer. Coordinated regulation of H2 fate and electrochemical electron transfer can effectively drive the preferential formation of vivianite, providing a new strategy for simultaneous phosphorus recovery and H2 accumulation from sludge.

Original languageEnglish
Article number126237
JournalWater Research
Volume303
DOIs
StatePublished - 15 Sep 2026
Externally publishedYes

Keywords

  • Chloroform
  • Electrode regulation
  • Electron transfer
  • Homoacetogenesis
  • Hydrogen reduction
  • Vivianite

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